25
SAGVNTVM (PLAV) 45 2013 25 - 38
ISSN 0210-3729
ISSN online 2174-517X
DOI 107203SAGVNTVM452007
Texto recibido el 01012013
Texto aceptado el 30052013
HVGH OD ORFDOLW]DFLy L H[FDYDFLy VLVWHPjWLFD GmiddotDV-sentaments a lrsquoaire lliure en les darreres degravecades el tre-
EDOO VREUH FRYHV KD SHUGXW FHUWD HPEUDQ]LGD HVSUpVGmiddotHQWHQGUH TXH HOV KjELWDWV L JUDQ SDUW GH OHV DFWLYLWDWVHFRQzPLTXHVVmiddotKDQGXWDWHUPHDOmiddotDLUHOOLXUHOHVFRYHVKDQTXHGDWVRYLQWOOLJDGHVDDFWLYLWDWVVHFXQGjULHVUHODFL-RQDGHV DPE OmiddotHPPDJDW]HPDWJH SH[ VLWJHVIRVVD D ODampRYD DPE OD WUDQVKXPjQFLD L HVWDEXODFLy SH[ampRYDampRORPHUDRampRYDGHODXLQHXRDPEODLQKXPDFLy
(p ex Cova de lrsquoAvellaner) entre drsquoaltres vinculades
drsquouna manera o altra a assentaments a lrsquoaire lliure Mo-
GHOVGmiddotDTXHVWHVWLOVmiddotKDQSURSRVDWSHU3ODQVDOORVDLODYDOOGHOOLHUFDRVFKRSHUOHVXL[HUHVGH9LOREtLlrsquoAlt Penedegraves (Mestres i Ribeacute 1992)
Al Prepirineu i Pirineu a lrsquooest del riu Segre les dades
VREUHSRVVLEOHVDVVHQWDPHQWVDOmiddotDLUHOOLXUHVyQPROWHVFDV-VHVLHVOLPLWHQDFHUWHVWUREDOOHVGHVFRQWH[WXDOLW]DGHVR WD-OOHUVGHVtOH[micro5RGDQpVL5DPyQ2PVet al 2009)
(QDTXHVWWUHEDOOHVSUHVHQWHQOHVGDGHVUHIHUHQWVDODampRYDampRORPHUD6DQW(VWHYHGHOD6DUJD3DOODUV-XVVjGXUDQWHO1HROtWLFFDUGLDOAgraveQDO$SDUWLUGHOVGLIHUHQWV VRQGHMRVGXWVD WHUPHGHVGH OmiddotDQ VmiddotKDSRJXWREVHUYDU ODYDULHWDWGmiddotXVRV L IXQFLRQDOLWDWVGHO MDFLPHQWHQPRPHQWVSRWHQFLDOPHQWVLQFUzQLFV3HUXQDEDQGDXQD]RQDRQSUHGRPLQHQOHVHVWUXFWXUHVGHFDLUHGRPqVWLFIRJDUVIRVVHVLIRUDWVGHSDOTXHHQVPRVWUHQOHVGDGHVHQWRUQOmiddotKjELWDWDOMDFLPHQWLSHUDOWUDEDQGDXQJUDQVHFWRUGHODFDYLWDWGHGLFDWDOmiddotHVWDEXODFLyGHUDPDWVDPEsediments de tipus IXPLHULSUREDEOHPHQWWDPEpDOmiddotHPPDJDW]HPDWJH7RWDL[zVXFFHHL[HQXQHVGDWDFLRQVGmiddotHQWUHL3$TXHVWHVGDGHVHVFRQWH[WXDOLW]HQDPEOHVGmiddotDOWUHVMDFLPHQWVGHOD]RQDSLULQHQFDXQjPELWTXHVHPSUHKDHVWDWGHAgraveQLWHQODELEOLRJUDAgraveDFRPXQHVSDLGHSDVHQWUHGLIHUHQWVELzWRSVHFROzJLFVGHOHVSODQHVIqUWLOVDOHVSDVWXUHVGmiddotHVWLX
Paraules clauKjELWDWHQFRYDHVWDEXODFLy1HROtWLFDQWLF3UHSLULQHXGHOHLGD
CAVE SETTLEMENT AND HERDING SPACES CA 6200-6000 BP THE EARLY NEOLITHIC AT COVA COLOMERA (PRE-PYRENEES OF LLEIDA) PRELIMINARY RESULTS
7KLVSDSHUSUHVHQWVGDWDUHJDUGLQJampRYDampRORPHUD6DQW(VWHYHGHOD6DUJD3DOODUV-XVVjGXULQJWKHODWHampDUGLDOSKDVH(DUO1HROLWKLFDVHGRQGLIIHUHQWDUFKDHRORJLFDOAgraveQGVFDUULHGRXWVLQFHWKHGLIIHUHQWXVHVDQGIXQFWLRQDOLWLHVRIWKLVVLWHLQSRWHQWLDOOVQFKURQRXVtimes have been observed On the one hand an area where domestic structures prevail (hearths pits and postholes) which shows data UHJDUGLQJ WKH OLYLQJVSDFHV$OWKRXJKWDJUHDWVHFWRURI WKHFDYLWZDVGHYRWHG WR WKHKRXVLQJRIKHUGVZLWKVHGLPHQWVRIPDQXUH WSHIXPLHUDQGSUREDEODOVRGHYRWHGWRVWRUDJH7KHVHHYHQWVRFFXUZLWKLQWKHHDUV37KHVHGDWDDUHFRQWH[WXDOLVHGE IXUWKHUGDWDRIRWKHU VLWHV LQ WKH3UHQHDQDUHDDQDWXUDO UHJLRQ WKDWKDVDOZDVEHHQGHAgraveQHG LQ WKHELEOLRJUDSKDVDFURVVLQJVLWHIRUGLIIHUHQWHFRORJLFDOELRWRSHVRIWKHIHUWLOHSODLQVLQWKHVXPPHUSDVWXUHV
Key wordsFDYHKDELWDWKRXVLQJ(DUO1HROLWKLF3UH3UHQHHVRIOHLGD
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL
NEOLIacuteTIC ANTIC
F XAVIER OMS JUAN M LOacutePEZ-GARCIacuteA XAVIER MANGADO PATRICIA MARTIN SUSANA MENDIELA
-8$1025$(605($3(52$11$525Igrave8(=shy$7$525Igrave8(=amp17$60$5$lt8(52
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HVRSFLRQVSHUH[SOLFDUDTXHVWDPDQFDGHMDFLPHQWVVyQGXHVSRVVLEOHIDOWDGHSURVSHFFLyRGmiddotREUHVYLjULHVRGmiddotXQWLSXVVLPLODUTXHQmiddotKDJLQIDFLOLWDWODWUREDOODRKjELWDWGLV-SHUVTXHQRQHFHVVLWDULDGHJUDQVDVVHQWDPHQWVTXHKDJLQGHL[DW HPSUHPWHV acuteDUTXHROzJLTXHVmicro GmiddotHQWLWDW HQ DTXHVWVWHUULWRULV3HUDTXHVWPRWLX OmiddotH[FDYDFLyGHFDYLWDWVFRQWL-QXDVHQWOmiddot~QLFDPDQHUDGHFDUDFWHULW]DUHOVWLSXVGmiddotDFWLYLWDWKXPDQDHQDTXHVWD]RQD(QDTXHVWVHQWLWOHVGDGHVFRPHQ-
FHQDVHULPSRUWDQWVHVGHODGqFDGDGHOVDQVGHOVVREUHWRWD$UDJyVmiddotKDQH[FDYDWXQLPSRUWDQWQRPEUHGHMDFLPHQWVHQWUHHOVTXDOVGHVWDTXHQODampXHYDGHampKDYHVODampXHYDGHO0RURGH2OYHQDROmiddot(VSOXJDGHOD3XDVFDGDHQWUHPROWVGmiddotDOWUHV$ampDWDOXQDOHVGDGHVKDQHVWDWPH-QRUVSHUzHQHOVGDUUHUVDQVVmiddotKDQLQFUHPHQWDWGHPDQHUDimportant amb la recerca a la Cova del Parco la Cova Gran
GH6DQWDLQDRODampRYDampRORPHUDHQWUHGmiddotDOWUHV0ROWVDOWUHVMDFLPHQWVMDFRQHJXWVGHVGHOVLLQLFLVGHOPRVWUHQGDGHVVREUHOmiddotRFXSDFLyGHO3UHSLULQHXDOmiddotRHVWGHOULX6HJUHWRWLTXHQRFRPSWHQDPEGDGHVHVWUDWLJUjAgraveTXHV(Oms et al 2012) Malauradament les dades disponibles
GHMDFLPHQWVDOmiddotDLUHOOLXUHFRQWLQXHQVHQWTXDVLQXOAtildeOHVVLH[FHSWXHPHOVFDVRVGH3ODQVDOORVDRVFKet al 1999) i la
Font del Ros (Pallareacutes et al 1997) al Prepirineu oriental
FDWDOjLHOVMDFLPHQWVGH7RUUROOyQL)RUQLOORVDO3UHSLULQHXdrsquoOsca (Utrilla 2012)
LA COVA COLOMERA CONTEXT GEOGRAgraveFIC I GEOLOgraveGIC
Al liacutemit occidental del Prepirineu de Lleida (Catalu-
QDWUREHPOD6HUUDGHO0RQWVHFXQHVSDLQDWXUDODPESURWHFFLySDUFLDOLTXHDPLGDXQVNPGHOODUJHQVHQWLW(2FRQYHUWLQWVHHQXQDXWqQWLFPXUTXHVHSDUDOHVSOD-QHVGHOHLGDDO6LODampRQFDGH7UHPSMXVWDEDQVGHOV3LULQHXVDO1DVHUUDWpXQDPLWMDGmiddotDOoDGDGmiddotHQWUHHOVPVQPLDVVROHL[XQDDOWXUDPj[LPDGHPDOSLFGH6DQW$OtVHVYDOOVTXHHVOOLXUHQDO0RQWVHFHVWUREHQDPVQPSHO6YDOOGmiddotshyJHULPVQPSHON (vall de Sant Esteve) La serra del Montsec es troba
tallada perpendicularment per tres rius (drsquoO a E Noguera
5LEDJRUoDQD1RJXHUD 3DOODUHVD L RL[ TXH KDQ REHUWVHQJOHVFRQJRVWV0RQWUHEHL7HUUDGHWV L3DV1RXTXHKDQ HVWDW SDVVRV FOjVVLFV SHU OD WUDYHVVD GH OD VHUUD(OQRPEUHGHMDFLPHQWVSUHKLVWzULFVHQDTXHVWD]RQDpVPROWHOHYDWLFRPSUqQGHVGHO3DOHROtWLFPLWMjAgraveQVHOAgraveQDOGHOmiddotHGDWGHOURQ]H2PVet al 2009)
La Cova Colomera situada al bell mig del Congost
de Montrebei a una alccedilada de 670 msnm i a 150 m per
sobre el riu teacute unes coordenades UTM (31N ED50) de
ltAgraveJ$DFDYLWDWpVUHVXOWDWGHOmiddotHURVLySDUFLDOGmiddotXQSDTXHW
GHFDOFjULHVVHFXQGjULHVGHO0DDVWULFKWLjLGHJUDQSDUWGmiddotXQD GLjFODVL GmiddotRULHQWDFLy1(62 (OV SURFHVVRV Ej-VLFVGHODVHYDHYROXFLyVyQXQDSULPHUDIDVHGmiddotREHUWXUDDPE SUHGRPLQL GmiddotDJHQWV GH FRUURVLyGLVROXFLy SURFH-GHQWVGHOHVAgraveOWUDFLRQVGHODSODWDIRUPDVXSHULRUSURSHUDa la carena de la serra i una segona de caiguda de blocs
SHUGHVFDOFLAgraveFDFLyGHOVHVWUDWV$OJXQVGmiddotDTXHVWVIHQz-
PHQVVyQGHJUDQPDJQLWXGLSURYRTXHQJUDQVDFXPXOD-FLRQVGHEORFVHQGLIHUHQWVVHFWRUVGHODFRYDHVVHYHVGLPHQVLRQVVyQPGmiddotDOWSHUGmiddotDPSODGDHQODERFDprincipal i una galeria de 180 m de llarg amb una alccedila-
GDPLWMDQDGHPHQWRWDODFRYDDFRYDSUHVHQWDXQYHVWtEXODPSOLLOOXPLQyVHQHOSXQWWRSRJUjAgraveFPpVelevat amb un espai planer drsquouns 60 m
2URGHMDWGHJUDQVEORFVHVWUXFWXUDOV$SDUWLUGmiddotDTXHVWSXQWVmiddotLQLFLDODJUDQJDOHULDHQXQDSHQGHQWPLWMDGmiddotXQVTXHDVVROHL[HOAgraveQDOGHODFDYLWDWDPGHOYHVWtEXO8QDDOWUDSH-
tita boca es troba a lrsquoinici de la portada principal de la
FRYD(VWUDFWDGmiddotXQDJDOHULDDVFHQGHQWTXHPHQDDXQFRUULROTXHWUDQVFRUUHGXUDQWPWRWDOPHQWSHQMDWVR-
EUHHOFRQJRVWDPEXQDDPSODGDPj[LPDGHPLTXHSRUWD D OD EDVH GmiddotXQ WRUUHQW DUUDQF GH0DWDPDOD DPVQP$TXHVWD ]RQD VLWXDGD D VREUH GH OD FRYD
)LJRFDOLW]DFLyLSODQWDGHOMDFLPHQWDPELQGLFDFLyGHOVVRQGH-MRVamp(Lamp9
27
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
GyQDDFFpVDOVFRQWUDIRUWVERVFRVRVGmiddotREDJDGHO0RQW-VHF L D SHWLWHV YDOOV L ]RQHV GH EDOPHV DL[t FRP D ODPlana de Montrebei (entre 920 i 974 msnm)
CONTEXT CULTURAL I CRONOLOgraveGIC
La Cova Colomera es troba integrada en un grup de
MDFLPHQWVGHO3LULQHXL3UHSLULQHXHQWUHODYDOOGHO6HJUHLOD]RQDGmiddot2VFDUDQSDUWGmiddotDTXHVWVDVVHQWDPHQWVHVPHQ-
WDWV D OD LQWURGXFFLy VHJXHL[HQ XQHV SDXWHV VLPLODUV HQTXDQW D UHJLVWUH FHUjPLF L D GDWDFLRQV UDGLRFDUEzQLTXHVHV FDUDFWHUtVWLTXHV PpV EjVLTXHV KDQ HVWDW UHFHQWPHQWDQDOLW]DGHV2PVet al 2012)
SHUFHQWDWJHVPHQRUVDOGHGHFRUDFLyFDUGLDOSURIXVLyGHOHVGHFRUDFLRQVLPSUHVHVGmiddotLQVWUXPHQW
(c 30-50)
- inici de les decoracions acanalades
UHSUHVHQWDFLyGHGHFRUDFLRQVLQFLVRLPSUHVHVGHWL-SXVERTXLTXH
- continuiumltat amb les sintaxis decoratives meacutes simples
del Neoliacutetic cardial
IRUTXLOODFURQROzJLFDDSUR[LPDGD3$TXHVWVWUHWVHVWUREHQSUHVHQWVHQMDFLPHQWVFRPOD
Cova del Parco (Petit 1996) Cueva de Chaves Ia i Cueva
GHO0RUR GH2OYHQD acuteFiPDUD VXSHULRUmicro 5DPyQ DL[tFRPHQGmiddotDOWUHVMDFLPHQWVDOVXGLQRUGGHOV3LULQHXV
Pel cas particular de la Cova Colomera tot i algunes
SHWLWHVGLIHUqQFLHVHQHOV UHJLVWUHVGHOVGLIHUHQWVQLYHOOVGHO1HROtWLFDQWLFFUHLHPTXHPRVWUHQXQPDWHL[KRULW]yprou homogeni (Oms 2008) Les datacions radiocarbograveni-
TXHV GLVSRQLEOHV AgraveJ PRVWUHQ DTXHVWD GLQjPLFD QRREVWDQW OD GDWD GHO QLYHOO amp( PRVWUD XQD GLVSHUVLyOOHXJHUDPHQWDOOXQDGDGHODUHVWDSHUzHOUHJLVWUHGLVSR-
QLEOHpVGHOWRWKRPRJHQLAgraveJLSRVVLEOHPHQWDTXHVWDGDWDFLyPRVWUDULDXQODSVHAgraveQDOGHODIDVHDTXtDQDOLW]DGD
)LJ0DWHULDOVFHUjPLFVGHOQHROtWLFDQWLFGHOVVRQGHMRVamp(Lamp9
)LJDWDFLRQVGHOVQLYHOOVGHO1HROtWLFDQWLFGHODampRYDampRORPHUDFDOLEUDGHVPLWMDQoDQWHOVRIWZDUHampDO3DOmiddotFRUED+XO~
28
F XAVIER OMS JUAN M LOacutePEZ-GARCIacuteA XAVIER MANGADO PATRICIA MARTIN SUSANA MENDIELA JUAN I MORALES MIREIA PEDROANNA RODRIacuteGUEZ AgraveGATA RODRIacuteGUEZ-CINTAS MARIA YUBERO
ELS AgraveMBITS DE LA COVA
HVGHOmiddotDQDODampRYDampRORPHUDVmiddotKDQREHUWGRVVRQGHMRVDUTXHROzJLFV1AgraveJXQGmiddotHOOVDOD]RQDdel vestiacutebul de la cavitat (Sondeig CV) en la part topo-
JUjAgraveFDPHQWPpVHOHYDGDGHODFDYLWDWPHQWUHTXHOmiddotDOWUHVmiddotKDUHDOLW]DWDODGUHWDGHODSULPHUDJUDQVDODGHODFDYL-WDW6RQGHLJamp(VREUHXQJUDQWDO~VTXHHQIRUPDGHventall davalla del vestiacutebul i arriba amb una moderada
SHQGHQWAgraveQVHOAgraveQDOGHODSULPHUDJUDQVDOD(VWDQDOOX-
QDWVDPEGyVVRQGHMRV~QLFDPHQWSHUVLVPHWUHVSHUzHQHVSDLV FRPSOHWDPHQWGLIHUHQWVmiddotHOHFFLyGHOV HVSDLV HVYDUHDOLW]DUDSDUWLUGHOHVH[FDYDFLRQVQRUHJXODGHVGXWHVDWHUPHDODFRYDGXUDQWODGqFDGDGHOVDQVGHOSDVVDWVHJOH H OD9HJD$TXHVWV WUHEDOOV SUHWqULWV YDQIRUQLUXQFRQMXQWGHPDWHULDOVPROWH[WHQVSHUzVHQVHFDSFRQWH[WHVWUDWLJUjAgraveFAgraveDEOHWDQWGHODampRYDampRORPHUDFRPGmiddotDOWUHVMDFLPHQWVGHODVHUUDGHO0RQWVHFLKDQHVWDWUH-visats recentment per nosaltres (Oms et al 2009)
621(amp((63$middot(67$8$ampETH
Els nivells del Neoliacutetic antic de la Cova Colomera
srsquoestenen en aproximadament 13 m2 del Sondeig CE (Co-
ORPHUD(VW$TXHVWHVSDLHVFRUUHVSRQDPEODSDUWEDL[DGHOWDO~VVHGLPHQWDULTXHIRUPDHOFRQGHOYHVWtEXOYHUVlrsquointerior de la cavitat
6middotKDQLGHQWLAgraveFDWAgraveQVHOPRPHQWWUHVQLYHOOVDUTXHROz-
JLFVFRUUHVSRQHQWVDDTXHVWD IDVHamp(amp( Lamp((Oms et alHOVTXDOVHVSUHVHQWHQGHPDQHUDPpV
RPHQVKRULW]RQWDOWRWLTXHDPEDOJXQHVSHUWRUEDFLRQVKDELWXDOV HQ DTXHVW WLSXV GH VHGLPHQWV R QLYHOOV FRPFDXV FORWV GH IXUWLXV R HVWUXFWXUHV SUHKLVWzULTXHV FRPXQDVLWMDIRVVDGHOURQ]HDQWLF2PVet al 2009) o un
UHWDOOLUUHJXODUGHO1HROtWLFAgraveQDO9HUD]LjQLYHOOamp(GR-
FXPHQWDWDOVTXDGUHVLlt(OV WUHV QLYHOOV QHROtWLFV GRFXPHQWDWV VyQGH WLSXV
fumierpVDGLUQLYHOOVGmiddotHVWDEXODFLyGHUDPDWV$TXHVWVUHVSRQHQDXQDFRPSRVLFLyRUJjQLFDGmiddotHVIHUzOLWVAgraveWzOLWVGLDWRPHHVDJUHJDWVFULVWDOAtildeOLQVHWFDGDO$OMD-FLPHQWVmiddotLGHQWLAgraveTXHQFRPXQDVXSHUSRVLFLyGHFDSHVGHGLIHUHQWVFRORUVTXHYDQGHVGHOQHJUHEDL[DWHPSHUDWX-
UDAgraveQVDOEODQFVHGLPHQWFDOFLQDWSDVVDQWSHOVYHUPHOOVUXEDIHFWDWVPDUURQVLJULVRV
(VSHQVDTXHDTXHVWWLSXVGHGLSzVLWpVSURGXwWSHUODFUHPD PpV R PHQV VLVWHPjWLFD L LQWHQVLYD GH IHPVGmiddotKHUEHVIXOOHVUHVWHVGHIXVWDLGmiddotDOWUHVHOHPHQWVGHUL-vats de lrsquoactivitat ramadera desenvolupada a la cavitat
HUJDGjURFKLHUDGDO$OOXpHPDQHUDSUHOLPLQDUHVSRWDAgraveUPDUTXHOHVPRVWUHVGHPLFURPRUIRORJLDGHODampRORPHUDSUHVHQWHQXQDWRWDOVLQ-
FURQLDDPEDTXHVWDFRPSRVLFLyVmiddotREVHUYDDSDUWGHUHVL-GXVYHJHWDOVFDUERQRVRVXQDDFXPXODFLyGHFHQGUHVYH-JHWDOVPROWGLYHUVLAgraveFDGHVndashIXOOHVUHVWHVOOHQRVHVHWFndash i
elements drsquoorigen excremental ovicapriacute (com pers Mer-
FqHUJDGj7RWLTXHHOGHEDWFRQWLQXDREHUWHVSURSRVDTXH ODAgraveQDOLWDWGDUUHUDVLJXL OmiddotHOLPLQDFLy LQWHQFLRQDOGHUHVLGXVH[FUHPHQWVLSDUjVLWVHOVTXDOVSRGLHQDIHFWDUODsalubritat i lrsquohabitabilitat de la cova per part dels grups
KXPDQVHUJDGjet al 2005 Angelucci et al 2009) No
REVWDQW DOJXQV DXWRUV SXQWXDOLW]HQ TXH GHSHQHQW GH ODORFDOLW]DFLy L IUHTHQWDFLy GH OD FDYLWDW FRP D FOHGDDTXHVWVUHVLGXVSRGULHQVLPSOHPHQWVHUDEDQGRQDWVLFRQ-
VHTHQWPHQWSHUGULHQYROXPLSUHVqQFLDGHPDWHULDORU-JjQLF JUjFLHV D RUJDQLVPHV FRSUzIDJV 9HUGDVFR DGDOL$WLHQ]D
middotREMHFWLXpVDPpVGHGHWHUPLQDUHOVGLIHUHQWVPR-
PHQWV GH FRPEXVWLy TXH SHU FRQYHQFLy HV GHQRPLQHQQLYHOOVWDPEpLQGLYLGXDOLW]DUFDGDWRQDOLWDWGHFRORUIj-cies) normalment amb poc desenvolupament lateral
$TXHVWDGHJUDGDFLyFURPjWLFDVHPEODUHVSRQGUHDGLIH-rents temperatures assolides a lrsquointerior de lrsquoamuntega-
PHQWGHIHPVLFRQVHTHQWPHQWHOVPDWHULDOVDUTXHROzJLFVHV YHXUDQPpV RPHQV DIHFWDWV HQ OD VHYD FRQVHUYDFLyGHSHQHQWGHOHVIjFLHVRQKDJLQHVWDWORFDOLW]DWV
(OVWUHVQLYHOOVDUTXHROzJLFVFRPSWHQDPEXQDSRWqQ-
FLDGHVLJXDOGHSHQHQWGHOD]RQDGHOVRQGHLJLGHIHWHQFHUWV TXDGUHV DOJXQV GmiddotDTXHVWV QLYHOOV HV WUREHQ PROW
)LJ3DUWGHOmiddotHVWUDWLJUDAgraveDGHamp(DOTXDGUHSUHSDUDFLyGHPRVWUDPLFURPRUIROzJLFD$GDOW D ODGUHWD IXOOHVGHERL[ L WLJHVvegetals en el contacte entre el nivell CE14 i el plistocegrave CE15 A
baix a la dreta amb macro
29
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de la cavitat amb caigudes de grans blocs (nivell CE11)
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ralesa cendrosa de tots els nivells i per tant de la seva
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WLSXVGHGLSzVLWpVOmiddotDSOLFDGDDOmiddotH[FDYDFLyGHODampXHYDGHO0LUDGRURQHVVLVWHPDWLW]DODSUHVqQFLDGHQLYHOOVDSDUWLUGHODGHVFULSFLyGHOHVGLIHUHQWVIjFLHVGRFXPHQWDGHVRE-
VHUYDQWVH VHPSUH XQ FDUjFWHU UHSHWLWLX HQ OD GLVSRVLFLyGmiddotDTXHVWVQLYHOOVFUHPDWV9HUJqVet al 2008 Angelucci et alampDGDQLYHOOHVWjFRPSRVWSHUXQJUXSGHIjFLHVTXHHVUHSHWHL[HQVHPSUHDPEODPDWHL[DGLVSRVLFLy$ODEDVHOHVIjFLHVc r o m carbonoses perograve sense massa im-
SDFWH WqUPLF DO VRVWUH OHV IjFLHVb o J molt calcinades
HQWUHPLJ GLIHUHQWV IjFLHV TXH UHVSRQHQ DOV JUDGLHQWV GHFUHPDFLyHQDXJPHQWGHVRVWUHDEDVHampDGDFLFOHFRP-
SOHWpVGHAgraveQLWFRPXQQLYHOO$QLYHOOWDIRQzPLFVLEpDOsostre de CE12 srsquoobserven materials meacutes moderns proce-
GHQWVGHOWUHSLJVXEDFWXDOLGHODIDVH6XS5HPODUHVWDGHQLYHOOVSHUPHWHQDVVHJXUDUXQDFRUUHFWDGLVSRVLFLyHVWUDWL-JUjAgraveFDHQJHQHUDOSRFDOWHUDGDFRQQH[LRQVDQDWzPLTXHVin situ IUDJPHQWVFHUjPLFV WUHQFDWVSHUSUHVVLySHUzQRVHSDUDWVHWF(OVFDXVVyQHOVDJHQWVGHGLVWRUVLyPpVHYL-dents en el seu interior el sediment apareix solt amb les
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UHVWHV GHPLFURYHUWHEUDWV$OWUHV GLVWRUVLRQV GH FDUjFWHUSUHKLVWzULF VyQ OHV IjFLHV tf TXH WDPEp UHVSRQHQ D XQDDPDOJDPDGHGLIHUHQWVIjFLHVORFDOLW]DGHVHQERVVDGHVLQRen llantions El seu origen ens eacutes indeterminat malgrat
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dria indicar la curta permanegravencia a la cova no obstant la
SUHVqQFLDGHPROLQVIUDFWXUDWVHQOmiddotHVWUDWGHQHWHMDGHOD(ampLHQOmiddotDERFDPHQWGmiddotDPRUWLW]DFLyGHODIRVVDFRQWH-nidor 9 ens parlaria drsquoactivitats estables a la cova De la
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SDULHQHQODLGHDGmiddotXQKjELWDWVHPLSHUPDQHQW$TXHVWWLSXVGmiddotHVWUXFWXUHVTXHDUWLFXOHQOmiddotHVSDLRFX-
SDWHQFRYDHVWUREHQHQDOWUHVMDFLPHQWV(OVIRJDUVLOHVIRVVHV GH IXQFLy GLYHUVD VyQ HOV PpV KDELWXDOV DPEexemples com la Cova de les Cendres la Cova del Vidre
HUJDGj OD DOPD 0DUJLQHGD XLODLQH L0DUW]OXIIODampRYDUDQGH6DQWDLQD0RUDet alRODampRYDRVFKHQWUHPROWVGmiddotDO-WUHV(QFDQYLOHVHVWUXFWXUHVPpVFRPSOH[HVTXHHVSR-
den correspondre amb cabanes o tancats dins de coves
compta amb exemples meacutes escassos com les cabanes de
ODDOPHGH5RQ]H7KLUDXOWLHHFKLQJRODGROLQDGH5RFDGRXUDVFyL0XOOHU
Al sondeig CE la presegravencia de nivells de tipus fumier
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35
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
espai drsquoaproximadament 20 m2 pels nivells CE 13 i
amp( ampRP VmiddotKD GLW DTXHVW jPELW KDXULD HVWDW HPSUDWFRPDPtQLPHQWUHVIDVHVPRPHQWVHQTXHVmiddotKDXULDHV-tabulat ramats i posteriorment srsquohaurien amuntegat els
VHXVIHPVLSRVVLEOHPHQWLQFHQGLDWDEDQVGmiddotDEDQGRQDUODcavitat A nivell orientatiu les datacions mostren una no-
table proximitat entre els nivellsmoments CE13 i CE14
LDOPDWHL[WHPSVOHVGDGHVDUTXHR]RROzJLTXHVLQGLTXHQFLFOHVFRPSOHWVGmiddotHVWDEXODFLyDPEFULDin situ) en els ni-
vells CE12 i CE14
6LFRPVmiddotKD LQVLVWLW OmiddotDFWLYLWDWHQWUH OHV]RQHVamp9Lamp(QRVHULDVLPXOWjQLDSHUzVtGLDFUzQLFDPHQWFRPSOH-PHQWjULD HV SRW GHGXLU TXH GXUDQW OD IDVH GHO1HROtWLFantic a la Cova Colomera srsquohi van produir un miacutenim de
FLQFPRPHQWVGmiddotRFXSDFLyGRVUHODFLRQDWVDPEXQKjELWDWVHPLSHUPDQHQWLWUHVDPEPRPHQWVGmiddot~VGHODFRYDFRPDFOHGDSHUUDPDWV(QDTXHVWVHQWLW ODampRYDampRORPHUDpodria ser un assentament complementari amb usos es-
SHFLDOLW]DWVGHSHQHQWGHODqSRFDRGHODIDVH3UREDEOH-PHQWODIDVHPpVDQWLJDGHOVRQGHLJamp9LHOQLYHOOamp(es correspondrien amb moments drsquoestada meacutes curts
PHQWUHTXH OD VHJRQD IDVHGHO VRQGHLJamp9 LHOVQLYHOOVCE14 i CE12 es relacionarien amb unes estades meacutes in-
WHQVHVLPpVOODUJXHV(QDTXHVWVHQWLWHVGHVFRQHL[VLHVFRUUHVSRQGULHQ DPE JUXSV LWLQHUDQWV GHPDMRU HVFDOD RDPEJUXSVSHUPDQHQWVDOD]RQDLGHPRELOLWDWUHGXwGD
UacuteS DE LES COVES PIRINENQUES
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VHVWRV TXH QR VyQ GHWHFWDWV R OLPLWDWV HQ HO FDPS 3HUDTXHVWPRWLXpVPROWSUREDEOHTXHODPDMRULDGHFDYLWDWVKDJLQHVWDWHPSUDGHVSHUPpVGmiddotXQDIXQFLyFRPHQoDQWSHUXQVLPSOHUHIXJLRELYDFSXQWXDORDOWUHVDFWLYLWDWVVLPLODUVTXHSRGHQGHL[DUXQDHPSUHPWD LPSHUFHSWLEOH8QDOWUHSUREOHPDTXHGLAgraveFXOWDODFDUDFWHULW]DFLyGHOVXVRVGHOHVFDYLWDWVpVODSRFDLQIRUPDFLyTXHHVSRVVHHL[SURFHGHQWGmiddotH[FDYDFLRQVUHFHQWVAgraveJ
)LJ6LWXDFLyGHOVMDFLPHQWVGHOQHROtWLFDQWLFDOmiddotRHVWGHOULX6HJUH
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EODFLRQVGHOD]RQDGXUDQWHO1HROtWLFDQWLFLSHUODQHROLWLW-]DFLyGHOWHUULWRULDOGHOORXL8WULOOD8WULOOD6middotKLKDQGRFXPHQWDWGLYHUVHVIRVVHVGHGHVIHWVIRUDWVGHSDOIRJDUVSRVVLEOHVVzOVGmiddotRFXSDFLyLLQFO~VXQHQWHUUD-PHQWHQIRVVDFREHUWSHUFzGROVLUHVWHVKXPDQHVGLVSHUVHVpels nivells (Utrilla et al8QDOWUHMDFLPHQWFOjVVLFGH OD UHJLy pV HO$EULJRGH ODV)RUFDV UDXV2VFD$TXHVWDEDOPDSUHVHQWDXQDOODUJDVHTqQFLDHQWUHOmiddot(SL-SDOHROtWLFLHOampDOFROtWLFHQHOVQLYHOOV9L9RQWRWLTXHQRHVGRFXPHQWDXQDHVWUXFWXUDFLyFRPSOH[DGHOmiddotHVSDLHVSURSRVDDSDUWLUGHOHVUHVWHVOtWLTXHVLODIDXQDH[FOXVLYD-PHQWVDOYDWJHTXHHVWUDFWDULDGmiddotXQDVVHQWDPHQWDPEXQDFODUDIXQFLyFLQHJqWLFD8WULOODL0D]R
$OWUHVMDFLPHQWVGHOD]RQDDUDJRQHVDSRGULHQKDYHUproporcionat dades al respecte perograve malauradament no
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3XDVFDGDRODampXHYDGHOD0LUDQGDHQWUHGmiddotDOWUHV8WUL-OODHQGmiddotDOWUHVFDVRVOHVGDGHVVyQHQFDUDSUHOLPL-QDUVFRPSHUODampXHYDGHOV7URFV5RMRet al 2012)
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$O WHUULWRUL FDWDOj D SDUW GH ODampRYDampRORPHUD D ODampRYDGHO3DUFR$OzVGHDODJXHUVmiddotKLGRFXPHQWjHQOHVH[FDYDFLRQVGHO6(53XQDVLWMDIRVVD((GHO1HROtWLFDQWLFampDUGLDOAgraveQDOH[FDYDGDHQHOVQLYHOOVHSLSDOHROtWLFV$SDUWLUGHOmiddotHVWXGLPLFURPRUIROzJLFGmiddotDTXHVWDHVWUXFWXUDHVYDSRGHUGHGXLUOmiddotHPPDJDW]HPDWJHDODFDYLWDWLOmiddotHVWDEX-
ODFLyGHUDPDWV3HWLW(O)RUDWGHODampRQTXHWDOHV$YHOODQHV6DQWDLQDSHWLWDFDYLWDWDPEXQGLSzVLWVH-pulcral molt important del IIIr milmiddotlenni comptava amb un
QLYHOOEDVDO DPE UHVWHV FHUjPLTXHVHSLFDUGLDOV DPEXQHVPRUIRORJLHVLFDUDFWHUtVWLTXHVTXHVHPEODYHQLQGLFDUTXHHVSRGULD WUDFWDUGmiddotXQHVSDLGHVWLQDWD OmiddotHPPDJDW]H-PDWJHHQJUDQVYDVRVRQ]iOH]0DUFpQet alIDF-WRUTXHHVYHXULDFRUURERUDWSHUOHVFRQGLFLRQVGHODFRYDDampRYDUDQGH6DQWDLQDOHV$YHOODQHV6DQWDLQDGRFXPHQWDXQHVSDLDPEPXOWLWXGGmiddotHVWUXFWXUHVGRPqVWLTXHV
IRJDUVIRUDWVGHSDOUHWDOOVLQGHWHUPLQDWVVLWJHVIRVVHVDOJXQD GH OHV TXDOV Wp XQD FURQRORJLD GHO1HROtWLF DQWLF(Mora et al 2011)
$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-
UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
ampRORPHUDRQHOFRQMXQWGHGDWDFLRQV UDGLRFDUEzQLTXHVSHUPHWSURSRVDUTXHODIXQFLyGmiddotKjELWDWFRPSOH[LGmiddotHV-SDLGmiddotHVWDEXODFLyYDQVHUPROWSURSHUVHQHOWHPSVWRWLTXHQRVLQFUzQLTXHV3HUDTXHVWPRWLXWRWLODLPSRUWjQFLDLQGXEWDEOHGHSREODWVGHPpVRPHQVPDJQLWXGDOJXQHVFRYHVDPEFDUDFWHUtVWLTXHVHVSHFLDOVVHULHQXQSXQWLP-
portant en la vida dels grups humans
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1 (OVWUHEDOOVDUTXHROzJLFVDODampRYDampRORPHUDHVGXHQDWHUPHHQel context del grup de recerca consolidat SERP (SGR2009-
GH OD 8QLYHUVLWDW GH DUFHORQD middotHVSDL QDWXUDO RQ HVWUREDHOMDFLPHQWSHUWDQDOmiddotshyUHDGH7HUULWRULL0HGL$PELHQWGHampDWDOXQDampDL[DTXH VHPSUHKD FROAtildeODERUDW DFWLYDPHQW HQUHFXUVRVHFRQzPLFVLLQIUDHVWUXFWXUHVWDPEpKDPRVWUDWXQJUDQinteregraves en tot moment Agraiumlm a Toni Nievas tot el suport durant
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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PETIT M (eacuted) (1996) El proceacutes de neolititzacioacute a la Vall del Se-JUHDampRYDGHO3DUFR$OzVGHDODJXHU(VWXGLGHOHVocupacions humanes del Vegrave al II milmiddotlenni aCDUFHORQD
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ROVIRA J CURA M (1992) Observacions sobre alguns materials
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LA COVA COLOMERA CONTEXT GEOGRAgraveFIC I GEOLOgraveGIC
Al liacutemit occidental del Prepirineu de Lleida (Catalu-
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tallada perpendicularment per tres rius (drsquoO a E Noguera
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La Cova Colomera situada al bell mig del Congost
de Montrebei a una alccedilada de 670 msnm i a 150 m per
sobre el riu teacute unes coordenades UTM (31N ED50) de
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CONTEXT CULTURAL I CRONOLOgraveGIC
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del Neoliacutetic cardial
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dria indicar la curta permanegravencia a la cova no obstant la
SUHVqQFLDGHPROLQVIUDFWXUDWVHQOmiddotHVWUDWGHQHWHMDGHOD(ampLHQOmiddotDERFDPHQWGmiddotDPRUWLW]DFLyGHODIRVVDFRQWH-nidor 9 ens parlaria drsquoactivitats estables a la cova De la
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SDULHQHQODLGHDGmiddotXQKjELWDWVHPLSHUPDQHQW$TXHVWWLSXVGmiddotHVWUXFWXUHVTXHDUWLFXOHQOmiddotHVSDLRFX-
SDWHQFRYDHVWUREHQHQDOWUHVMDFLPHQWV(OVIRJDUVLOHVIRVVHV GH IXQFLy GLYHUVD VyQ HOV PpV KDELWXDOV DPEexemples com la Cova de les Cendres la Cova del Vidre
HUJDGj OD DOPD 0DUJLQHGD XLODLQH L0DUW]OXIIODampRYDUDQGH6DQWDLQD0RUDet alRODampRYDRVFKHQWUHPROWVGmiddotDO-WUHV(QFDQYLOHVHVWUXFWXUHVPpVFRPSOH[HVTXHHVSR-
den correspondre amb cabanes o tancats dins de coves
compta amb exemples meacutes escassos com les cabanes de
ODDOPHGH5RQ]H7KLUDXOWLHHFKLQJRODGROLQDGH5RFDGRXUDVFyL0XOOHU
Al sondeig CE la presegravencia de nivells de tipus fumier
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35
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
espai drsquoaproximadament 20 m2 pels nivells CE 13 i
amp( ampRP VmiddotKD GLW DTXHVW jPELW KDXULD HVWDW HPSUDWFRPDPtQLPHQWUHVIDVHVPRPHQWVHQTXHVmiddotKDXULDHV-tabulat ramats i posteriorment srsquohaurien amuntegat els
VHXVIHPVLSRVVLEOHPHQWLQFHQGLDWDEDQVGmiddotDEDQGRQDUODcavitat A nivell orientatiu les datacions mostren una no-
table proximitat entre els nivellsmoments CE13 i CE14
LDOPDWHL[WHPSVOHVGDGHVDUTXHR]RROzJLTXHVLQGLTXHQFLFOHVFRPSOHWVGmiddotHVWDEXODFLyDPEFULDin situ) en els ni-
vells CE12 i CE14
6LFRPVmiddotKD LQVLVWLW OmiddotDFWLYLWDWHQWUH OHV]RQHVamp9Lamp(QRVHULDVLPXOWjQLDSHUzVtGLDFUzQLFDPHQWFRPSOH-PHQWjULD HV SRW GHGXLU TXH GXUDQW OD IDVH GHO1HROtWLFantic a la Cova Colomera srsquohi van produir un miacutenim de
FLQFPRPHQWVGmiddotRFXSDFLyGRVUHODFLRQDWVDPEXQKjELWDWVHPLSHUPDQHQWLWUHVDPEPRPHQWVGmiddot~VGHODFRYDFRPDFOHGDSHUUDPDWV(QDTXHVWVHQWLW ODampRYDampRORPHUDpodria ser un assentament complementari amb usos es-
SHFLDOLW]DWVGHSHQHQWGHODqSRFDRGHODIDVH3UREDEOH-PHQWODIDVHPpVDQWLJDGHOVRQGHLJamp9LHOQLYHOOamp(es correspondrien amb moments drsquoestada meacutes curts
PHQWUHTXH OD VHJRQD IDVHGHO VRQGHLJamp9 LHOVQLYHOOVCE14 i CE12 es relacionarien amb unes estades meacutes in-
WHQVHVLPpVOODUJXHV(QDTXHVWVHQWLWHVGHVFRQHL[VLHVFRUUHVSRQGULHQ DPE JUXSV LWLQHUDQWV GHPDMRU HVFDOD RDPEJUXSVSHUPDQHQWVDOD]RQDLGHPRELOLWDWUHGXwGD
UacuteS DE LES COVES PIRINENQUES
(OUHAacuteH[VREUHOHVDFWLYLWDWVUHDOVTXHHVGXLHQDWHUPHHQXQMDFLPHQWRQLYHOOQRSRGHQVHUFRQHJXGHVDPEHOQLYHOOGHODUHFHUFDDFWXDOMDTXHXQQRPEUHLQGHAgraveQLWGHYDULDEOHVTXDQWDODIXQFLySRGHQFRQIRQGUHmiddotVHQSDOLPS-
VHVWRV TXH QR VyQ GHWHFWDWV R OLPLWDWV HQ HO FDPS 3HUDTXHVWPRWLXpVPROWSUREDEOHTXHODPDMRULDGHFDYLWDWVKDJLQHVWDWHPSUDGHVSHUPpVGmiddotXQDIXQFLyFRPHQoDQWSHUXQVLPSOHUHIXJLRELYDFSXQWXDORDOWUHVDFWLYLWDWVVLPLODUVTXHSRGHQGHL[DUXQDHPSUHPWD LPSHUFHSWLEOH8QDOWUHSUREOHPDTXHGLAgraveFXOWDODFDUDFWHULW]DFLyGHOVXVRVGHOHVFDYLWDWVpVODSRFDLQIRUPDFLyTXHHVSRVVHHL[SURFHGHQWGmiddotH[FDYDFLRQVUHFHQWVAgraveJ
)LJ6LWXDFLyGHOVMDFLPHQWVGHOQHROtWLFDQWLFDOmiddotRHVWGHOULX6HJUH
36
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EODFLRQVGHOD]RQDGXUDQWHO1HROtWLFDQWLFLSHUODQHROLWLW-]DFLyGHOWHUULWRULDOGHOORXL8WULOOD8WULOOD6middotKLKDQGRFXPHQWDWGLYHUVHVIRVVHVGHGHVIHWVIRUDWVGHSDOIRJDUVSRVVLEOHVVzOVGmiddotRFXSDFLyLLQFO~VXQHQWHUUD-PHQWHQIRVVDFREHUWSHUFzGROVLUHVWHVKXPDQHVGLVSHUVHVpels nivells (Utrilla et al8QDOWUHMDFLPHQWFOjVVLFGH OD UHJLy pV HO$EULJRGH ODV)RUFDV UDXV2VFD$TXHVWDEDOPDSUHVHQWDXQDOODUJDVHTqQFLDHQWUHOmiddot(SL-SDOHROtWLFLHOampDOFROtWLFHQHOVQLYHOOV9L9RQWRWLTXHQRHVGRFXPHQWDXQDHVWUXFWXUDFLyFRPSOH[DGHOmiddotHVSDLHVSURSRVDDSDUWLUGHOHVUHVWHVOtWLTXHVLODIDXQDH[FOXVLYD-PHQWVDOYDWJHTXHHVWUDFWDULDGmiddotXQDVVHQWDPHQWDPEXQDFODUDIXQFLyFLQHJqWLFD8WULOODL0D]R
$OWUHVMDFLPHQWVGHOD]RQDDUDJRQHVDSRGULHQKDYHUproporcionat dades al respecte perograve malauradament no
FRPSWHQDPEHVWUDWLJUDAgraveHVGHOWRWAgraveDEOHVRSURXH[FDYD-des com la Cueva del Moro de Olvena lrsquoEspluga de la
3XDVFDGDRODampXHYDGHOD0LUDQGDHQWUHGmiddotDOWUHV8WUL-OODHQGmiddotDOWUHVFDVRVOHVGDGHVVyQHQFDUDSUHOLPL-QDUVFRPSHUODampXHYDGHOV7URFV5RMRet al 2012)
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$O WHUULWRUL FDWDOj D SDUW GH ODampRYDampRORPHUD D ODampRYDGHO3DUFR$OzVGHDODJXHUVmiddotKLGRFXPHQWjHQOHVH[FDYDFLRQVGHO6(53XQDVLWMDIRVVD((GHO1HROtWLFDQWLFampDUGLDOAgraveQDOH[FDYDGDHQHOVQLYHOOVHSLSDOHROtWLFV$SDUWLUGHOmiddotHVWXGLPLFURPRUIROzJLFGmiddotDTXHVWDHVWUXFWXUDHVYDSRGHUGHGXLUOmiddotHPPDJDW]HPDWJHDODFDYLWDWLOmiddotHVWDEX-
ODFLyGHUDPDWV3HWLW(O)RUDWGHODampRQTXHWDOHV$YHOODQHV6DQWDLQDSHWLWDFDYLWDWDPEXQGLSzVLWVH-pulcral molt important del IIIr milmiddotlenni comptava amb un
QLYHOOEDVDO DPE UHVWHV FHUjPLTXHVHSLFDUGLDOV DPEXQHVPRUIRORJLHVLFDUDFWHUtVWLTXHVTXHVHPEODYHQLQGLFDUTXHHVSRGULD WUDFWDUGmiddotXQHVSDLGHVWLQDWD OmiddotHPPDJDW]H-PDWJHHQJUDQVYDVRVRQ]iOH]0DUFpQet alIDF-WRUTXHHVYHXULDFRUURERUDWSHUOHVFRQGLFLRQVGHODFRYDDampRYDUDQGH6DQWDLQDOHV$YHOODQHV6DQWDLQDGRFXPHQWDXQHVSDLDPEPXOWLWXGGmiddotHVWUXFWXUHVGRPqVWLTXHV
IRJDUVIRUDWVGHSDOUHWDOOVLQGHWHUPLQDWVVLWJHVIRVVHVDOJXQD GH OHV TXDOV Wp XQD FURQRORJLD GHO1HROtWLF DQWLF(Mora et al 2011)
$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-
UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
ampRORPHUDRQHOFRQMXQWGHGDWDFLRQV UDGLRFDUEzQLTXHVSHUPHWSURSRVDUTXHODIXQFLyGmiddotKjELWDWFRPSOH[LGmiddotHV-SDLGmiddotHVWDEXODFLyYDQVHUPROWSURSHUVHQHOWHPSVWRWLTXHQRVLQFUzQLTXHV3HUDTXHVWPRWLXWRWLODLPSRUWjQFLDLQGXEWDEOHGHSREODWVGHPpVRPHQVPDJQLWXGDOJXQHVFRYHVDPEFDUDFWHUtVWLTXHVHVSHFLDOVVHULHQXQSXQWLP-
portant en la vida dels grups humans
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1 (OVWUHEDOOVDUTXHROzJLFVDODampRYDampRORPHUDHVGXHQDWHUPHHQel context del grup de recerca consolidat SERP (SGR2009-
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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Fig 6 Planta de les ocupacions del neo-
liacutetic antic del Sondeig CV
31
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LES DADES ARQUEOZOOLOgraveGIQUES
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tracta de la espegravecie salvatge o beacute la domegravestica
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Les dades preliminars del sondeig CE mostren varie-
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35
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gis puntuals (Cova del Sardo Cova del Pas de la Lloba
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CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
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PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
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26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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34
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35
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AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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GUILAINE J MARTZLUFF M (1995) Les excavacions a la DOPDGHOD0DUJLQHGD Andorra
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Fig 6 Planta de les ocupacions del neo-
liacutetic antic del Sondeig CV
31
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vells CE12 i CE14
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$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-
UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
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HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
ampRORPHUDRQHOFRQMXQWGHGDWDFLRQV UDGLRFDUEzQLTXHVSHUPHWSURSRVDUTXHODIXQFLyGmiddotKjELWDWFRPSOH[LGmiddotHV-SDLGmiddotHVWDEXODFLyYDQVHUPROWSURSHUVHQHOWHPSVWRWLTXHQRVLQFUzQLTXHV3HUDTXHVWPRWLXWRWLODLPSRUWjQFLDLQGXEWDEOHGHSREODWVGHPpVRPHQVPDJQLWXGDOJXQHVFRYHVDPEFDUDFWHUtVWLTXHVHVSHFLDOVVHULHQXQSXQWLP-
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
26amp+shy(O1HROtWLFRDQWLJXRHQHOQRUGHVWHGHampDWDOXxDampRQWULEXFLyQDODSUREOHPiWLFDGHODHYROXFLyQGHODVSUL-meras comunidades neoliacuteticas del Mediterraacuteneo occiden-
tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
52amp+(5-((QYLURQPHQWDOLPSDFWRI1HROLWKLFDQGURQ]H$JHIDUPLQJLQWKHHDVWHUQ3UHQHHVIRUHODQGVED-VHGRQPXOWLGLVFLSOLQDULQYHVWLJDWLRQVDWDampDXQHGHp-OHVWD pOHVWD ampDYH QHDU 3HUSLJQDQ )UDQFH9HJHWDWLRQHistory and Archaeobotany 7 1-9
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GUILAINE J MARTZLUFF M (1995) Les excavacions a la DOPDGHOD0DUJLQHGD Andorra
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PETIT M (eacuted) (1996) El proceacutes de neolititzacioacute a la Vall del Se-JUHDampRYDGHO3DUFR$OzVGHDODJXHU(VWXGLGHOHVocupacions humanes del Vegrave al II milmiddotlenni aCDUFHORQD
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de la EC-1 coberts tots per un mateix estrat Es desco-
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IUDJPHQWVGmiddotXQPDWHL[YDVDUHGyVGHOD(ampLOD(ampTXHSRGULHQPRVWUDUXQDVLQFURQLDRXQDPDWHL[DDPRUWLW]DFLy HQWUH OHV HVWUXFWXUHV (OV IUDJPHQWV GH OD
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VHYD DPRUWLW]DFLy WDPEpYD VHU SUREDEOHPHQW FRHWjQLDPosteriorment al seu segellament es van obrir dos petits
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dria indicar la curta permanegravencia a la cova no obstant la
SUHVqQFLDGHPROLQVIUDFWXUDWVHQOmiddotHVWUDWGHQHWHMDGHOD(ampLHQOmiddotDERFDPHQWGmiddotDPRUWLW]DFLyGHODIRVVDFRQWH-nidor 9 ens parlaria drsquoactivitats estables a la cova De la
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SDULHQHQODLGHDGmiddotXQKjELWDWVHPLSHUPDQHQW$TXHVWWLSXVGmiddotHVWUXFWXUHVTXHDUWLFXOHQOmiddotHVSDLRFX-
SDWHQFRYDHVWUREHQHQDOWUHVMDFLPHQWV(OVIRJDUVLOHVIRVVHV GH IXQFLy GLYHUVD VyQ HOV PpV KDELWXDOV DPEexemples com la Cova de les Cendres la Cova del Vidre
HUJDGj OD DOPD 0DUJLQHGD XLODLQH L0DUW]OXIIODampRYDUDQGH6DQWDLQD0RUDet alRODampRYDRVFKHQWUHPROWVGmiddotDO-WUHV(QFDQYLOHVHVWUXFWXUHVPpVFRPSOH[HVTXHHVSR-
den correspondre amb cabanes o tancats dins de coves
compta amb exemples meacutes escassos com les cabanes de
ODDOPHGH5RQ]H7KLUDXOWLHHFKLQJRODGROLQDGH5RFDGRXUDVFyL0XOOHU
Al sondeig CE la presegravencia de nivells de tipus fumier
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35
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
espai drsquoaproximadament 20 m2 pels nivells CE 13 i
amp( ampRP VmiddotKD GLW DTXHVW jPELW KDXULD HVWDW HPSUDWFRPDPtQLPHQWUHVIDVHVPRPHQWVHQTXHVmiddotKDXULDHV-tabulat ramats i posteriorment srsquohaurien amuntegat els
VHXVIHPVLSRVVLEOHPHQWLQFHQGLDWDEDQVGmiddotDEDQGRQDUODcavitat A nivell orientatiu les datacions mostren una no-
table proximitat entre els nivellsmoments CE13 i CE14
LDOPDWHL[WHPSVOHVGDGHVDUTXHR]RROzJLTXHVLQGLTXHQFLFOHVFRPSOHWVGmiddotHVWDEXODFLyDPEFULDin situ) en els ni-
vells CE12 i CE14
6LFRPVmiddotKD LQVLVWLW OmiddotDFWLYLWDWHQWUH OHV]RQHVamp9Lamp(QRVHULDVLPXOWjQLDSHUzVtGLDFUzQLFDPHQWFRPSOH-PHQWjULD HV SRW GHGXLU TXH GXUDQW OD IDVH GHO1HROtWLFantic a la Cova Colomera srsquohi van produir un miacutenim de
FLQFPRPHQWVGmiddotRFXSDFLyGRVUHODFLRQDWVDPEXQKjELWDWVHPLSHUPDQHQWLWUHVDPEPRPHQWVGmiddot~VGHODFRYDFRPDFOHGDSHUUDPDWV(QDTXHVWVHQWLW ODampRYDampRORPHUDpodria ser un assentament complementari amb usos es-
SHFLDOLW]DWVGHSHQHQWGHODqSRFDRGHODIDVH3UREDEOH-PHQWODIDVHPpVDQWLJDGHOVRQGHLJamp9LHOQLYHOOamp(es correspondrien amb moments drsquoestada meacutes curts
PHQWUHTXH OD VHJRQD IDVHGHO VRQGHLJamp9 LHOVQLYHOOVCE14 i CE12 es relacionarien amb unes estades meacutes in-
WHQVHVLPpVOODUJXHV(QDTXHVWVHQWLWHVGHVFRQHL[VLHVFRUUHVSRQGULHQ DPE JUXSV LWLQHUDQWV GHPDMRU HVFDOD RDPEJUXSVSHUPDQHQWVDOD]RQDLGHPRELOLWDWUHGXwGD
UacuteS DE LES COVES PIRINENQUES
(OUHAacuteH[VREUHOHVDFWLYLWDWVUHDOVTXHHVGXLHQDWHUPHHQXQMDFLPHQWRQLYHOOQRSRGHQVHUFRQHJXGHVDPEHOQLYHOOGHODUHFHUFDDFWXDOMDTXHXQQRPEUHLQGHAgraveQLWGHYDULDEOHVTXDQWDODIXQFLySRGHQFRQIRQGUHmiddotVHQSDOLPS-
VHVWRV TXH QR VyQ GHWHFWDWV R OLPLWDWV HQ HO FDPS 3HUDTXHVWPRWLXpVPROWSUREDEOHTXHODPDMRULDGHFDYLWDWVKDJLQHVWDWHPSUDGHVSHUPpVGmiddotXQDIXQFLyFRPHQoDQWSHUXQVLPSOHUHIXJLRELYDFSXQWXDORDOWUHVDFWLYLWDWVVLPLODUVTXHSRGHQGHL[DUXQDHPSUHPWD LPSHUFHSWLEOH8QDOWUHSUREOHPDTXHGLAgraveFXOWDODFDUDFWHULW]DFLyGHOVXVRVGHOHVFDYLWDWVpVODSRFDLQIRUPDFLyTXHHVSRVVHHL[SURFHGHQWGmiddotH[FDYDFLRQVUHFHQWVAgraveJ
)LJ6LWXDFLyGHOVMDFLPHQWVGHOQHROtWLFDQWLFDOmiddotRHVWGHOULX6HJUH
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EODFLRQVGHOD]RQDGXUDQWHO1HROtWLFDQWLFLSHUODQHROLWLW-]DFLyGHOWHUULWRULDOGHOORXL8WULOOD8WULOOD6middotKLKDQGRFXPHQWDWGLYHUVHVIRVVHVGHGHVIHWVIRUDWVGHSDOIRJDUVSRVVLEOHVVzOVGmiddotRFXSDFLyLLQFO~VXQHQWHUUD-PHQWHQIRVVDFREHUWSHUFzGROVLUHVWHVKXPDQHVGLVSHUVHVpels nivells (Utrilla et al8QDOWUHMDFLPHQWFOjVVLFGH OD UHJLy pV HO$EULJRGH ODV)RUFDV UDXV2VFD$TXHVWDEDOPDSUHVHQWDXQDOODUJDVHTqQFLDHQWUHOmiddot(SL-SDOHROtWLFLHOampDOFROtWLFHQHOVQLYHOOV9L9RQWRWLTXHQRHVGRFXPHQWDXQDHVWUXFWXUDFLyFRPSOH[DGHOmiddotHVSDLHVSURSRVDDSDUWLUGHOHVUHVWHVOtWLTXHVLODIDXQDH[FOXVLYD-PHQWVDOYDWJHTXHHVWUDFWDULDGmiddotXQDVVHQWDPHQWDPEXQDFODUDIXQFLyFLQHJqWLFD8WULOODL0D]R
$OWUHVMDFLPHQWVGHOD]RQDDUDJRQHVDSRGULHQKDYHUproporcionat dades al respecte perograve malauradament no
FRPSWHQDPEHVWUDWLJUDAgraveHVGHOWRWAgraveDEOHVRSURXH[FDYD-des com la Cueva del Moro de Olvena lrsquoEspluga de la
3XDVFDGDRODampXHYDGHOD0LUDQGDHQWUHGmiddotDOWUHV8WUL-OODHQGmiddotDOWUHVFDVRVOHVGDGHVVyQHQFDUDSUHOLPL-QDUVFRPSHUODampXHYDGHOV7URFV5RMRet al 2012)
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$O WHUULWRUL FDWDOj D SDUW GH ODampRYDampRORPHUD D ODampRYDGHO3DUFR$OzVGHDODJXHUVmiddotKLGRFXPHQWjHQOHVH[FDYDFLRQVGHO6(53XQDVLWMDIRVVD((GHO1HROtWLFDQWLFampDUGLDOAgraveQDOH[FDYDGDHQHOVQLYHOOVHSLSDOHROtWLFV$SDUWLUGHOmiddotHVWXGLPLFURPRUIROzJLFGmiddotDTXHVWDHVWUXFWXUDHVYDSRGHUGHGXLUOmiddotHPPDJDW]HPDWJHDODFDYLWDWLOmiddotHVWDEX-
ODFLyGHUDPDWV3HWLW(O)RUDWGHODampRQTXHWDOHV$YHOODQHV6DQWDLQDSHWLWDFDYLWDWDPEXQGLSzVLWVH-pulcral molt important del IIIr milmiddotlenni comptava amb un
QLYHOOEDVDO DPE UHVWHV FHUjPLTXHVHSLFDUGLDOV DPEXQHVPRUIRORJLHVLFDUDFWHUtVWLTXHVTXHVHPEODYHQLQGLFDUTXHHVSRGULD WUDFWDUGmiddotXQHVSDLGHVWLQDWD OmiddotHPPDJDW]H-PDWJHHQJUDQVYDVRVRQ]iOH]0DUFpQet alIDF-WRUTXHHVYHXULDFRUURERUDWSHUOHVFRQGLFLRQVGHODFRYDDampRYDUDQGH6DQWDLQDOHV$YHOODQHV6DQWDLQDGRFXPHQWDXQHVSDLDPEPXOWLWXGGmiddotHVWUXFWXUHVGRPqVWLTXHV
IRJDUVIRUDWVGHSDOUHWDOOVLQGHWHUPLQDWVVLWJHVIRVVHVDOJXQD GH OHV TXDOV Wp XQD FURQRORJLD GHO1HROtWLF DQWLF(Mora et al 2011)
$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-
UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
ampRORPHUDRQHOFRQMXQWGHGDWDFLRQV UDGLRFDUEzQLTXHVSHUPHWSURSRVDUTXHODIXQFLyGmiddotKjELWDWFRPSOH[LGmiddotHV-SDLGmiddotHVWDEXODFLyYDQVHUPROWSURSHUVHQHOWHPSVWRWLTXHQRVLQFUzQLTXHV3HUDTXHVWPRWLXWRWLODLPSRUWjQFLDLQGXEWDEOHGHSREODWVGHPpVRPHQVPDJQLWXGDOJXQHVFRYHVDPEFDUDFWHUtVWLTXHVHVSHFLDOVVHULHQXQSXQWLP-
portant en la vida dels grups humans
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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dria indicar la curta permanegravencia a la cova no obstant la
SUHVqQFLDGHPROLQVIUDFWXUDWVHQOmiddotHVWUDWGHQHWHMDGHOD(ampLHQOmiddotDERFDPHQWGmiddotDPRUWLW]DFLyGHODIRVVDFRQWH-nidor 9 ens parlaria drsquoactivitats estables a la cova De la
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SDULHQHQODLGHDGmiddotXQKjELWDWVHPLSHUPDQHQW$TXHVWWLSXVGmiddotHVWUXFWXUHVTXHDUWLFXOHQOmiddotHVSDLRFX-
SDWHQFRYDHVWUREHQHQDOWUHVMDFLPHQWV(OVIRJDUVLOHVIRVVHV GH IXQFLy GLYHUVD VyQ HOV PpV KDELWXDOV DPEexemples com la Cova de les Cendres la Cova del Vidre
HUJDGj OD DOPD 0DUJLQHGD XLODLQH L0DUW]OXIIODampRYDUDQGH6DQWDLQD0RUDet alRODampRYDRVFKHQWUHPROWVGmiddotDO-WUHV(QFDQYLOHVHVWUXFWXUHVPpVFRPSOH[HVTXHHVSR-
den correspondre amb cabanes o tancats dins de coves
compta amb exemples meacutes escassos com les cabanes de
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Al sondeig CE la presegravencia de nivells de tipus fumier
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35
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
espai drsquoaproximadament 20 m2 pels nivells CE 13 i
amp( ampRP VmiddotKD GLW DTXHVW jPELW KDXULD HVWDW HPSUDWFRPDPtQLPHQWUHVIDVHVPRPHQWVHQTXHVmiddotKDXULDHV-tabulat ramats i posteriorment srsquohaurien amuntegat els
VHXVIHPVLSRVVLEOHPHQWLQFHQGLDWDEDQVGmiddotDEDQGRQDUODcavitat A nivell orientatiu les datacions mostren una no-
table proximitat entre els nivellsmoments CE13 i CE14
LDOPDWHL[WHPSVOHVGDGHVDUTXHR]RROzJLTXHVLQGLTXHQFLFOHVFRPSOHWVGmiddotHVWDEXODFLyDPEFULDin situ) en els ni-
vells CE12 i CE14
6LFRPVmiddotKD LQVLVWLW OmiddotDFWLYLWDWHQWUH OHV]RQHVamp9Lamp(QRVHULDVLPXOWjQLDSHUzVtGLDFUzQLFDPHQWFRPSOH-PHQWjULD HV SRW GHGXLU TXH GXUDQW OD IDVH GHO1HROtWLFantic a la Cova Colomera srsquohi van produir un miacutenim de
FLQFPRPHQWVGmiddotRFXSDFLyGRVUHODFLRQDWVDPEXQKjELWDWVHPLSHUPDQHQWLWUHVDPEPRPHQWVGmiddot~VGHODFRYDFRPDFOHGDSHUUDPDWV(QDTXHVWVHQWLW ODampRYDampRORPHUDpodria ser un assentament complementari amb usos es-
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PHQWUHTXH OD VHJRQD IDVHGHO VRQGHLJamp9 LHOVQLYHOOVCE14 i CE12 es relacionarien amb unes estades meacutes in-
WHQVHVLPpVOODUJXHV(QDTXHVWVHQWLWHVGHVFRQHL[VLHVFRUUHVSRQGULHQ DPE JUXSV LWLQHUDQWV GHPDMRU HVFDOD RDPEJUXSVSHUPDQHQWVDOD]RQDLGHPRELOLWDWUHGXwGD
UacuteS DE LES COVES PIRINENQUES
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)LJ6LWXDFLyGHOVMDFLPHQWVGHOQHROtWLFDQWLFDOmiddotRHVWGHOULX6HJUH
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$OWUHVMDFLPHQWVGHOD]RQDDUDJRQHVDSRGULHQKDYHUproporcionat dades al respecte perograve malauradament no
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$O WHUULWRUL FDWDOj D SDUW GH ODampRYDampRORPHUD D ODampRYDGHO3DUFR$OzVGHDODJXHUVmiddotKLGRFXPHQWjHQOHVH[FDYDFLRQVGHO6(53XQDVLWMDIRVVD((GHO1HROtWLFDQWLFampDUGLDOAgraveQDOH[FDYDGDHQHOVQLYHOOVHSLSDOHROtWLFV$SDUWLUGHOmiddotHVWXGLPLFURPRUIROzJLFGmiddotDTXHVWDHVWUXFWXUDHVYDSRGHUGHGXLUOmiddotHPPDJDW]HPDWJHDODFDYLWDWLOmiddotHVWDEX-
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QLYHOOEDVDO DPE UHVWHV FHUjPLTXHVHSLFDUGLDOV DPEXQHVPRUIRORJLHVLFDUDFWHUtVWLTXHVTXHVHPEODYHQLQGLFDUTXHHVSRGULD WUDFWDUGmiddotXQHVSDLGHVWLQDWD OmiddotHPPDJDW]H-PDWJHHQJUDQVYDVRVRQ]iOH]0DUFpQet alIDF-WRUTXHHVYHXULDFRUURERUDWSHUOHVFRQGLFLRQVGHODFRYDDampRYDUDQGH6DQWDLQDOHV$YHOODQHV6DQWDLQDGRFXPHQWDXQHVSDLDPEPXOWLWXGGmiddotHVWUXFWXUHVGRPqVWLTXHV
IRJDUVIRUDWVGHSDOUHWDOOVLQGHWHUPLQDWVVLWJHVIRVVHVDOJXQD GH OHV TXDOV Wp XQD FURQRORJLD GHO1HROtWLF DQWLF(Mora et al 2011)
$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-
UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
ampRORPHUDRQHOFRQMXQWGHGDWDFLRQV UDGLRFDUEzQLTXHVSHUPHWSURSRVDUTXHODIXQFLyGmiddotKjELWDWFRPSOH[LGmiddotHV-SDLGmiddotHVWDEXODFLyYDQVHUPROWSURSHUVHQHOWHPSVWRWLTXHQRVLQFUzQLTXHV3HUDTXHVWPRWLXWRWLODLPSRUWjQFLDLQGXEWDEOHGHSREODWVGHPpVRPHQVPDJQLWXGDOJXQHVFRYHVDPEFDUDFWHUtVWLTXHVHVSHFLDOVVHULHQXQSXQWLP-
portant en la vida dels grups humans
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
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$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
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DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
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vells CE12 i CE14
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UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
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gis puntuals (Cova del Sardo Cova del Pas de la Lloba
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CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
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PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
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37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
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26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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PETIT M (eacuted) (1996) El proceacutes de neolititzacioacute a la Vall del Se-JUHDampRYDGHO3DUFR$OzVGHDODJXHU(VWXGLGHOHVocupacions humanes del Vegrave al II milmiddotlenni aCDUFHORQD
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33
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
LES DADES ARQUEOZOOLOgraveGIQUES
El seu estudi indica la predominanccedila de taxons do-
PqVWLFVHQDPEGyVVRQGHMRV$TXHVWJUXSHVWjFRPSRVWSHOV RYLFDSULQV TXH FRQVWLWXHL[HQPpV GHO GH OHVUHVWHVGHWHUPLQDGHVLSHOVEzYLGVTXHVXPHQPHQVGHOmiddotGHOHVUHVWHVLGHQWLAgraveFDGHVHQDPEGyVFRQMXQWV
(OVWD[RQVVDOYDWJHVVyQPROWSRFQRPEURVRVPHQVGHOGHOHVUHVWHVLGHQWLAgraveFDGHVHQHOVGRVFRQMXQWVcabirols (Capreolus capreolusODJRPRUIVFRQLOOVLOOH-EUHVLDXV(QHOFDVGHOVXLGVSUHVHQWVGHIRUPDPLQRUL-WjULDHQDPEGyVFRQMXQWVXQDUHVWDHQHOVRQGHLJamp9LVLVen el sondeig CE) no ha estat possible determinar si es
tracta de la espegravecie salvatge o beacute la domegravestica
3HOTXHIDDODUHSUHVHQWDFLyDQDWzPLFDHQHOVRQGHLJCE els ovicaprins estan representats per una bona part
GHOVHOHPHQWVGH OmiddotHVTXHOHWFUDQLDO LSRVWFUDQLDOPHQWUHTXH OD UHSUHVHQWDFLy GH OD UHVWD GH WD[RQV pVPROWPpVSDUFLDO(QHOFDVGHOVEzYLGVDTXHVWVHVWDQUHSUHVHQWDWVSHUDOJXQVHOHPHQWVGHOmiddotHVTXHOHWSRVWFUDQLDOLSHUQRPpVTXDWUHV HOHPHQWV GHO FUDQLDO TXDWUH GHQWV $TXHVWHVTXDWUH GHQWV HV WUREHQ DO QLYHOO amp( IHW TXH SRGULDUHODFLRQDUVH DPE XQ HVTXDUWHUDPHQW in situ GmiddotDTXHVWVDQLPDOVHQDTXHVWPRPHQWLGmiddotXQWUDQVSRUWGHOVPDWHL[RVals altres dos nivells CE13 i CE14
D UHSUHVHQWDFLy DQDWzPLFD SHU WD[RQV GHO VRQGHLJCV eacutes molt meacutes parcial degut al reduiumlt nombre de restes
LGHQWLAgraveFDGHV WD[RQzPLFDPHQW GmiddotXQ WRWDO GH HO$TXHVWIHW~QLFDPHQWH[SOLFDXQSURFHVVDWPD-MRU GH OHV UHVWHV D OD ]RQD GmiddotHVWUXFWXUHV GRPqVWLTXHV
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LES DADES CARPOLOgraveGIQUES
Les dades preliminars del sondeig CE mostren varie-
tat de cereals (7ULWLFXPDHVWLYXPGXUXP 7ULWLFXPGLFRF-cum 7ULWLFXP sp Hordeum sp) lleguminoses (Pisum sativum PisumVicia Vicia sp) aixiacute com restes de plan-
tes ruderals i adventiacutecies ($MXJDUHSWDQV o 7ULIROLXP sp)
LSDUWVVROWHVGHOVFHUHDOVEDVHVGmiddotHVSLJXHWDLIUDJPHQWVGHUDTXLV6LEpOmiddotHPPDJDW]HPDWJHGHJUDDODFDYLWDWQRpot ser corroborat encara de manera directa la presegravencia
GHUHVWHVSURFHGHQWVGHODQHWHMDGHOVFHUHDOVIUDJPHQWVGHUDTXLVLOHVEDVHVGmiddotHVSLJXHWDHQVSRGULHQHVWDULQGL-FDQWTXHODPzOWDGHOVFHUHDOVHVUHDOLW]DULDDODPDWHL[DFDYLWDW$TXHVWIHWHVYHXULDFRUURERUDWSHUODSUHVqQFLDGHPROLQVPDQVLPDW[XFDGRUVHQDPEGyVVRQGHMRVJDL-UHEpVHPSUHIUDFWXUDWVLWHUPRDOWHUDWV
)LJDGHVFDUSROzJLTXHVGHO6RQGHLJamp(GHODampRYDampRORPHUD
)LJ1RPEUHGHUHVWHVUHFXSHUDGHVHQDPEGyVFRQMXQWVGHampRYDampRORPHUDGLVWULEXwGHVSHUWD[yLFDWHJRULDGHWDOODGHSHV
34
F XAVIER OMS JUAN M LOacutePEZ-GARCIacuteA XAVIER MANGADO PATRICIA MARTIN SUSANA MENDIELA JUAN I MORALES MIREIA PEDROANNA RODRIacuteGUEZ AgraveGATA RODRIacuteGUEZ-CINTAS MARIA YUBERO
3HOTXHIDDODUHSUHVHQWDFLyWD[RQzPLFDLDIDOWDGHOVresultats del Sondeig CV la baixa presegravencia de restes del
QLYHOOamp(HVFRUUHVSRQDPEXQYROXPLQIHULRUGmiddotH[WHQ-
VLyFRQVLGHUDWOOLXUHGmiddotLQWUXVLRQVGHOQLYHOOVXSHUAgraveFLDOLSHUWDQWQRpVVLJQLAgraveFDWLXSHOPRPHQW(QFDQYLHOQLYHOOamp(DPEXQYROXPDQDOLW]DWVLPLODUDOGHamp(VtTXHSUHVHQWDXQQ~PHURGHUHVWHVPROWPHQRU$TXHVWIDFWRUSRGULDLQIHULUIXQFLRQVGLIHUHQWVSHUODFDYLWDWRXQRULJHQGLIHUHQWGHODPRVWUDFDUSROzJLFDGHSHQHQWGHODLQWHQVL-WDWGHODRFXSDFLy
USOS DE LrsquoESPAI
middotDSURAgraveWDPHQWGHOVHVSDLVGLVSRQLEOHVLODVHYDPRGL-AgraveFDFLyKDHVWDWWHVWLPRQLDGDDODampRYDampRORPHUDOmiddotKjELWDWLOmiddotHVWDEXODFLyGHUDPDWV3URSRVDUXQDSRVVLEOHFRHWDQH-iumltat entre les dues activitats no sembla a priori possible
MDTXHHVWUDFWDGHGRVXVRVQRFRPSOHPHQWDULVHQHOPD-WHL[PRPHQWSHUOHVLQFRPRGLWDWVTXHSURGXLULDOmiddotDFWLYLWDWGHO UDPDW DOV JUXSV KXPDQV SDUjVLWV LQVHFWHV RORUVetc) A meacutes les dades proporcionades pels materials ar-
TXHROzJLFV QR SHUPHWHQ LQIHULU FDS FRPSOHPHQWDULHWDWHQWUHHOVVHFWRUVGHOMDFLPHQW(QGmiddotDOWUHVFDVRVVmiddotKDQLQ-
IHULWWDPEpXVRVFRPSDUWLWVGHOmiddotHVSDLHQGLIHUHQWVIDVHVFRPODampRYDGHO3DUFRDPEXQDVLWMDDPRUWLW]DGDRQVmiddotKLGRFXPHQWDUHQUHVWHVGHIHPVGHUDPDWV3HWLW ODampRYDGHO9LGUHRQHVGRFXPHQWjHOPDWHL[UHVLGXHQXQDHVWUXFWXUD GH FRPEXVWLy HUJDGj R OD DOPDMargineda on es documentaren traces indirectes drsquoesta-
EXODFLyGHUDPDWVHQQLYHOOVGHVWLQDWVa priori a lrsquoemma-
JDW]HPDWJHLWDPEpDJUXSVGHFDLUHFLQHJqWLFXLODLQHL0DUW]OXII
3HOTXHIDDOmiddotKjELWDWVRQGHLJamp9ODIDVHGHO1HROt-tic antic de la Colomera compta amb nombroses estructu-
UHVQHJDWLYHVVRYLQWDIHFWDGHVSHUHVWUXFWXUHVGHODIDVHGHO URQ]H DQWLF 7RWHV DTXHVWHV HVWUXFWXUHV HV WUREHQYLQFXODGHVGHPDQHUDItVLFDDHVWUDWVTXHOHVFXUXOOHQRFREUHL[HQ 0DODXUDGDPHQW FRUUHODFLRQDU DTXHVWHV HV-tructures i els seus estrats amb drsquoaltres estructures de la
PDWHL[DIDVHpVFRPSOLFDW(OVFDVRVPpVHYLGHQWVVyQFLQFIRUDWVGHSDOGHPLGDSHWLWD)3DDUHGyV
de la EC-1 coberts tots per un mateix estrat Es desco-
QHL[DTXLQDGHOHVWUHVIDVHVGHFRPEXVWLyGRFXPHQWDGDHQHOIRJDUFRUUHVSRQHQ
IUDJPHQWVGmiddotXQPDWHL[YDVDUHGyVGHOD(ampLOD(ampTXHSRGULHQPRVWUDUXQDVLQFURQLDRXQDPDWHL[DDPRUWLW]DFLy HQWUH OHV HVWUXFWXUHV (OV IUDJPHQWV GH OD
(ampIRUHQGRFXPHQWDWVHQHOWHVWLPRQLGHODVHJRQDXWL-OLW]DFLyGHOIRJDU
OHVWUHVIRVVHVFRQWHQLGRU)ampDHVWUREHQH[FD-vades a lrsquointerior drsquoun mateix retall (UE303) i per tant la
VHYD DPRUWLW]DFLy WDPEpYD VHU SUREDEOHPHQW FRHWjQLDPosteriorment al seu segellament es van obrir dos petits
IRUDWVGHSDOMXVWDVREUHGHOHVHVWUXFWXUHVRULJLQDOV)313 i 14)
HOVIRUDWVGHSDOGHPLGDJUDQ)3Les troben parcialment alineats i coberts en gran part pel
PDWHL[ HVWUDW 8( L SRGULHQ IRUPDU XQD HVWUXFWXUDDqULD GH WHQGqQFLD TXDGUDQJXODU VL HV FRPELQHQ DPEGmiddotDOWUHV HOHPHQWV ) )3 L $TXHVWD SRVVLEOHHVWUXFWXUDDqULDGHJUDQPDJQLWXGYDVHUUHDOLW]DGDSRVWH-ULRUPHQWDOmiddotDPRUWLW]DFLyGHOIRJDU(amp
3HUWDQWHVSRWGHGXLUXQPtQLPGHGXHVIDVHVGLQVODXWLOLW]DFLyGHOD]RQDGHOVRQGHLJamp93HUXQFRVWDWGRVIRJDUV(ampL(ampMXQWDPEHOV)3DHQXQSULPHUPRPHQW SHU DOWUD EDQGD OD FRQVWUXFFLy GmiddotXQD SRVVLEOHJUDQ HVWUXFWXUD DqULD FDEDQD WDQFDW TXH DPRUWLW]DFRPDPtQLPOD(ampLHOVHXHVWUDWGHQHWHMD8($OWUHVHVWUXFWXUHVFRPOHVSRVVLEOHVIRVVHVFRQWHQLGRULHOIRJDU(ampVyQPpVGLItFLOVGHFRUUHODFLRQDUDPEDOJXQDGHOHVGXHVIDVHV(VWDEOLUODLQWHQVLWDWGmiddotDTXHVWDRFXSDFLyUHVXOWDFRPSOLFDWDPDQFDGH]RQHVGHWDOODin situ po-
dria indicar la curta permanegravencia a la cova no obstant la
SUHVqQFLDGHPROLQVIUDFWXUDWVHQOmiddotHVWUDWGHQHWHMDGHOD(ampLHQOmiddotDERFDPHQWGmiddotDPRUWLW]DFLyGHODIRVVDFRQWH-nidor 9 ens parlaria drsquoactivitats estables a la cova De la
PDWHL[D PDQHUD OD SUHVqQFLD GH IRJDUV UHXWLOLW]DWV LGmiddotHVWUDWV GH QHWHMD GH IRVVHVFRQWHQLGRU L AgraveQDOPHQWdrsquouna possible estructura aegraveria (cabana tancat) partici-
SDULHQHQODLGHDGmiddotXQKjELWDWVHPLSHUPDQHQW$TXHVWWLSXVGmiddotHVWUXFWXUHVTXHDUWLFXOHQOmiddotHVSDLRFX-
SDWHQFRYDHVWUREHQHQDOWUHVMDFLPHQWV(OVIRJDUVLOHVIRVVHV GH IXQFLy GLYHUVD VyQ HOV PpV KDELWXDOV DPEexemples com la Cova de les Cendres la Cova del Vidre
HUJDGj OD DOPD 0DUJLQHGD XLODLQH L0DUW]OXIIODampRYDUDQGH6DQWDLQD0RUDet alRODampRYDRVFKHQWUHPROWVGmiddotDO-WUHV(QFDQYLOHVHVWUXFWXUHVPpVFRPSOH[HVTXHHVSR-
den correspondre amb cabanes o tancats dins de coves
compta amb exemples meacutes escassos com les cabanes de
ODDOPHGH5RQ]H7KLUDXOWLHHFKLQJRODGROLQDGH5RFDGRXUDVFyL0XOOHU
Al sondeig CE la presegravencia de nivells de tipus fumier
HQXQjPELWOLPLWDWSHUEORFVHVWUXFWXUDOVODSUzSLDSDUHWGHODFDYLWDWLODSUHVqQFLDGHGRVIRUDWVGHSDOOLPLWHQXQ
35
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
espai drsquoaproximadament 20 m2 pels nivells CE 13 i
amp( ampRP VmiddotKD GLW DTXHVW jPELW KDXULD HVWDW HPSUDWFRPDPtQLPHQWUHVIDVHVPRPHQWVHQTXHVmiddotKDXULDHV-tabulat ramats i posteriorment srsquohaurien amuntegat els
VHXVIHPVLSRVVLEOHPHQWLQFHQGLDWDEDQVGmiddotDEDQGRQDUODcavitat A nivell orientatiu les datacions mostren una no-
table proximitat entre els nivellsmoments CE13 i CE14
LDOPDWHL[WHPSVOHVGDGHVDUTXHR]RROzJLTXHVLQGLTXHQFLFOHVFRPSOHWVGmiddotHVWDEXODFLyDPEFULDin situ) en els ni-
vells CE12 i CE14
6LFRPVmiddotKD LQVLVWLW OmiddotDFWLYLWDWHQWUH OHV]RQHVamp9Lamp(QRVHULDVLPXOWjQLDSHUzVtGLDFUzQLFDPHQWFRPSOH-PHQWjULD HV SRW GHGXLU TXH GXUDQW OD IDVH GHO1HROtWLFantic a la Cova Colomera srsquohi van produir un miacutenim de
FLQFPRPHQWVGmiddotRFXSDFLyGRVUHODFLRQDWVDPEXQKjELWDWVHPLSHUPDQHQWLWUHVDPEPRPHQWVGmiddot~VGHODFRYDFRPDFOHGDSHUUDPDWV(QDTXHVWVHQWLW ODampRYDampRORPHUDpodria ser un assentament complementari amb usos es-
SHFLDOLW]DWVGHSHQHQWGHODqSRFDRGHODIDVH3UREDEOH-PHQWODIDVHPpVDQWLJDGHOVRQGHLJamp9LHOQLYHOOamp(es correspondrien amb moments drsquoestada meacutes curts
PHQWUHTXH OD VHJRQD IDVHGHO VRQGHLJamp9 LHOVQLYHOOVCE14 i CE12 es relacionarien amb unes estades meacutes in-
WHQVHVLPpVOODUJXHV(QDTXHVWVHQWLWHVGHVFRQHL[VLHVFRUUHVSRQGULHQ DPE JUXSV LWLQHUDQWV GHPDMRU HVFDOD RDPEJUXSVSHUPDQHQWVDOD]RQDLGHPRELOLWDWUHGXwGD
UacuteS DE LES COVES PIRINENQUES
(OUHAacuteH[VREUHOHVDFWLYLWDWVUHDOVTXHHVGXLHQDWHUPHHQXQMDFLPHQWRQLYHOOQRSRGHQVHUFRQHJXGHVDPEHOQLYHOOGHODUHFHUFDDFWXDOMDTXHXQQRPEUHLQGHAgraveQLWGHYDULDEOHVTXDQWDODIXQFLySRGHQFRQIRQGUHmiddotVHQSDOLPS-
VHVWRV TXH QR VyQ GHWHFWDWV R OLPLWDWV HQ HO FDPS 3HUDTXHVWPRWLXpVPROWSUREDEOHTXHODPDMRULDGHFDYLWDWVKDJLQHVWDWHPSUDGHVSHUPpVGmiddotXQDIXQFLyFRPHQoDQWSHUXQVLPSOHUHIXJLRELYDFSXQWXDORDOWUHVDFWLYLWDWVVLPLODUVTXHSRGHQGHL[DUXQDHPSUHPWD LPSHUFHSWLEOH8QDOWUHSUREOHPDTXHGLAgraveFXOWDODFDUDFWHULW]DFLyGHOVXVRVGHOHVFDYLWDWVpVODSRFDLQIRUPDFLyTXHHVSRVVHHL[SURFHGHQWGmiddotH[FDYDFLRQVUHFHQWVAgraveJ
)LJ6LWXDFLyGHOVMDFLPHQWVGHOQHROtWLFDQWLFDOmiddotRHVWGHOULX6HJUH
36
F XAVIER OMS JUAN M LOacutePEZ-GARCIacuteA XAVIER MANGADO PATRICIA MARTIN SUSANA MENDIELA JUAN I MORALES MIREIA PEDROANNA RODRIacuteGUEZ AgraveGATA RODRIacuteGUEZ-CINTAS MARIA YUBERO
$$UDJyODampXHYDGHampKDYHVDVWDUiVampDVEDV2VFDpresenta en els nivells Ia Ib i I diversos usos i activitats
TXHPRVWUHQTXHIRXXQHQFODYDPHQWLPSRUWDQWSHUOHVSR-
EODFLRQVGHOD]RQDGXUDQWHO1HROtWLFDQWLFLSHUODQHROLWLW-]DFLyGHOWHUULWRULDOGHOORXL8WULOOD8WULOOD6middotKLKDQGRFXPHQWDWGLYHUVHVIRVVHVGHGHVIHWVIRUDWVGHSDOIRJDUVSRVVLEOHVVzOVGmiddotRFXSDFLyLLQFO~VXQHQWHUUD-PHQWHQIRVVDFREHUWSHUFzGROVLUHVWHVKXPDQHVGLVSHUVHVpels nivells (Utrilla et al8QDOWUHMDFLPHQWFOjVVLFGH OD UHJLy pV HO$EULJRGH ODV)RUFDV UDXV2VFD$TXHVWDEDOPDSUHVHQWDXQDOODUJDVHTqQFLDHQWUHOmiddot(SL-SDOHROtWLFLHOampDOFROtWLFHQHOVQLYHOOV9L9RQWRWLTXHQRHVGRFXPHQWDXQDHVWUXFWXUDFLyFRPSOH[DGHOmiddotHVSDLHVSURSRVDDSDUWLUGHOHVUHVWHVOtWLTXHVLODIDXQDH[FOXVLYD-PHQWVDOYDWJHTXHHVWUDFWDULDGmiddotXQDVVHQWDPHQWDPEXQDFODUDIXQFLyFLQHJqWLFD8WULOODL0D]R
$OWUHVMDFLPHQWVGHOD]RQDDUDJRQHVDSRGULHQKDYHUproporcionat dades al respecte perograve malauradament no
FRPSWHQDPEHVWUDWLJUDAgraveHVGHOWRWAgraveDEOHVRSURXH[FDYD-des com la Cueva del Moro de Olvena lrsquoEspluga de la
3XDVFDGDRODampXHYDGHOD0LUDQGDHQWUHGmiddotDOWUHV8WUL-OODHQGmiddotDOWUHVFDVRVOHVGDGHVVyQHQFDUDSUHOLPL-QDUVFRPSHUODampXHYDGHOV7URFV5RMRet al 2012)
$$QGRUUD ~QLFDPHQW HV FRQHL[ HO MDFLPHQW GH ODDOPD 0DUJLQHGD 6DQW -XOLj GH zULD $QGRUUD (QDTXHVW DVVHQWDPHQW HV GRFXPHQWDUHQ QRPEURVHV IRVVHVLUUHJXODUVGHIXQFLyLQGHWHUPLQDGDHQHOQLYHOO1HROtWLFDQWLFLTXHSHUIRUDYHQHOQLYHOO0HVROtWLFDL[tFRPHVWUXFWXUHVGHFRPEXVWLy6LEpVmiddotKDSXQWXDOLW]DWHQEDVHDODIDXQDGHODIDVHXQDIXQFLyFLQHJqWLFDSHOMDFLPHQWVmiddotKDQGRFXPHQWDW WDPEp WUDFHV LQGLUHFWHVGmiddotHVWDEXODFLyGHUDPDWVXLODLQHL0DUW]OXII
$O WHUULWRUL FDWDOj D SDUW GH ODampRYDampRORPHUD D ODampRYDGHO3DUFR$OzVGHDODJXHUVmiddotKLGRFXPHQWjHQOHVH[FDYDFLRQVGHO6(53XQDVLWMDIRVVD((GHO1HROtWLFDQWLFampDUGLDOAgraveQDOH[FDYDGDHQHOVQLYHOOVHSLSDOHROtWLFV$SDUWLUGHOmiddotHVWXGLPLFURPRUIROzJLFGmiddotDTXHVWDHVWUXFWXUDHVYDSRGHUGHGXLUOmiddotHPPDJDW]HPDWJHDODFDYLWDWLOmiddotHVWDEX-
ODFLyGHUDPDWV3HWLW(O)RUDWGHODampRQTXHWDOHV$YHOODQHV6DQWDLQDSHWLWDFDYLWDWDPEXQGLSzVLWVH-pulcral molt important del IIIr milmiddotlenni comptava amb un
QLYHOOEDVDO DPE UHVWHV FHUjPLTXHVHSLFDUGLDOV DPEXQHVPRUIRORJLHVLFDUDFWHUtVWLTXHVTXHVHPEODYHQLQGLFDUTXHHVSRGULD WUDFWDUGmiddotXQHVSDLGHVWLQDWD OmiddotHPPDJDW]H-PDWJHHQJUDQVYDVRVRQ]iOH]0DUFpQet alIDF-WRUTXHHVYHXULDFRUURERUDWSHUOHVFRQGLFLRQVGHODFRYDDampRYDUDQGH6DQWDLQDOHV$YHOODQHV6DQWDLQDGRFXPHQWDXQHVSDLDPEPXOWLWXGGmiddotHVWUXFWXUHVGRPqVWLTXHV
IRJDUVIRUDWVGHSDOUHWDOOVLQGHWHUPLQDWVVLWJHVIRVVHVDOJXQD GH OHV TXDOV Wp XQD FURQRORJLD GHO1HROtWLF DQWLF(Mora et al 2011)
$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-
UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-
gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
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IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC
FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
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DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
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GUILAINE J MARTZLUFF M (1995) Les excavacions a la DOPDGHOD0DUJLQHGD Andorra
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PETIT M (eacuted) (1996) El proceacutes de neolititzacioacute a la Vall del Se-JUHDampRYDGHO3DUFR$OzVGHDODJXHU(VWXGLGHOHVocupacions humanes del Vegrave al II milmiddotlenni aCDUFHORQD
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UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova
UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
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gis puntuals (Cova del Sardo Cova del Pas de la Lloba
HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD
CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-
PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy
37
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FRPSOH[DGHOmiddotHVSDLLTXHSRGULHQDMXGDUDYHUWHEUDUOmiddot~Vdel territori Aixiacute es pot demostrar en el cas de la Cova
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
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DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
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26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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GUILAINE J MARTZLUFF M (1995) Les excavacions a la DOPDGHOD0DUJLQHGD Andorra
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PETIT M (eacuted) (1996) El proceacutes de neolititzacioacute a la Vall del Se-JUHDampRYDGHO3DUFR$OzVGHDODJXHU(VWXGLGHOHVocupacions humanes del Vegrave al II milmiddotlenni aCDUFHORQD
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UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-
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gis puntuals (Cova del Sardo Cova del Pas de la Lloba
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CONCLUSIONS
La Cova Colomera esdeveacute un bon exemple drsquousos
complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW
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PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ
IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-
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BIBLIOGRAFIA
$8e(LQiPLFDGHODYHJHWDFLyQH[SORWDFLyQGHO-combustible lentildeoso durante el Pleistoceno Superior y el Holoceno del Noreste de la Peniacutensula Ibeacuterica a partir del DQiOLVLVDQWUDFROyJLFR Tesis doctoral inegravedita Universitat
Rovira i Virgili Tarragona
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DOI httpdxdoiorg10108000438240902843659
$$((OSRWHQFLDOSHFXDULRGHODYHJHWDFLyQPHGLWH-rraacutenea las cuevas redil $FWHVGHOampRQJUpVGHO1HROtWLFde la Peniacutensula Ibegraverica - HUQDEpX72UR]FR HGVValegravencia 69-76
$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH
(5$shy00$FWLYLGDGDQWUySLFDHQDOJXQDVVHFXHQ-
FLDVDUTXHROyJLFDVHQFXHYDGHO1HROtWLFRDQWLJXRFDWDOiQDWUDYpVGHODQiOLVLVPLFURPRUIROyJLFR7UDEDMRVGH3UHKLV-toria 54 (2) 151-161
DOI httpdxdoiorg103989tp1997v54i2372
(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
DOI httpdxdoiorg103989tp1994v51i1464
26amp+shy8ETH53$202$8amp+00$7(8-7$(51(52(amp$6$(9$ - El poblat neoliacutetic de Plansallosa Lrsquoexplotacioacute del territorio dels SULPHUVDJULFXOWRUVUDPDGHUVGHOmiddot$OWDDUURW[D Olot
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$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146
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(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU
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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75
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