h (p l n - core.ac.uk · gdwdfly prvwuduld xq odsvh Àqdo gh od idvh dtxt dqdolw]dgd )lj 0dwhuldov...

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

26

F XAVIER OMS JUAN M LOacutePEZ-GARCIacuteA XAVIER MANGADO PATRICIA MARTIN SUSANA MENDIELA JUAN I MORALES MIREIA PEDROANNA RODRIacuteGUEZ AgraveGATA RODRIacuteGUEZ-CINTAS MARIA YUBERO

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


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


DIHFWDWV SHU WUDPSOLQJV i per lrsquoepisodi drsquoabandonament

de la cavitat amb caigudes de grans blocs (nivell CE11)

TXH GLAgraveFXOWD HQ JUDQ SDUW OD GLIHUHQFLDFLy GHOV WUHV QL-YHOOV$L[tGRQFVDTXHVW IHWKDFRPSRUWDW ODGHVWUXFFLySDUFLDOGHODVHTqQFLDHQDOJXQVWUDPVDwOODWVFRPSHUH[HPSOHHQHOVTXDGUHV789DFDXVDGHODQDWX-

ralesa cendrosa de tots els nivells i per tant de la seva

IUDJLOLWDWDPHWRGRORJLDHPSUDGDSHUH[FDYDULGHVFULXUHDTXHVW

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

IjFLHVEDUUHMDGHV LTXHDGTXLUHL[HQXQFRORUJULVyVDPE

UHVWHV GHPLFURYHUWHEUDWV$OWUHV GLVWRUVLRQV GH FDUjFWHUSUHKLVWzULF VyQ OHV IjFLHV tf TXH WDPEp UHVSRQHQ D XQDDPDOJDPDGHGLIHUHQWVIjFLHVORFDOLW]DGHVHQERVVDGHVLQRen llantions El seu origen ens eacutes indeterminat malgrat

DL[z HV WUREHQ VHJHOODGHV SHU IjFLHV LQWDFWHV SHU DTXHVWmotiu podria tractar-se del resultat drsquoun trepig puntual

7DPEpMXJDDIDYRUGHODFRQVHUYDFLyGHOSDTXHWHQSRVLFLySULPjULD ODSUHVqQFLDGHIXOOHVGHERL[LAgraveEUHVEODQTXHVDPEPRUIRORJLDGHEUDQTXHVVREUHWRWHQHOFRQWDFWHHQWUHel nivell CE14 i el nivell plistocegrave CE15 potser a mode de

MDoRGHSDUWGHOmiddotDOLPHQWDFLyAgraveJ$FRQWLQXDFLyHVUHODWDODVHTqQFLDHVWUDWLJUjAgraveFDGHO

1HROtWLFDQWLFDO6RQGHLJamp(AgraveJ 1LYHOO amp( QLYHOO DUTXHROzJLF GRFXPHQWDW HQ

aproximadament 6 m2 FRQFUHWDPHQW HQ HOV TXDGUHV78LSDUWGHDVHYDSRWqQFLDYD-ULDHQWUHLFPGHSHQHQWGHOTXDGUHHVVHYHVIjFLHVVXSHULRUVHVWUREHQDIHFWDGHVSHUODSUHVqQFLDGHFODVWHVLblocs del nivell CE11 moment de caiguda de blocs de

VRVWUHLGmiddotDEDQGRQDPHQWGHODFDYLWDW(OVHXFLFOHGHIj-cies eacutes el meacutes reduiumlt de tots els presents es troba coronat

SHUXQDIjFLHVJ

- Nivell CE13 documentat en aproximadament 10

m2(QDOJXQVFDVRVVmiddotDMXQWDDPEHOQLYHOOamp(DOTXDOVHOLOOLXUDSHUVREUHDVHYDPj[LPDSRWqQFLDpVGHFPTXHHVGRFXPHQWDJHQHUDOPHQWHQOD]RQDPpVSRWHQWGHOWDO~VOtQLDGHOVTXDGUHVampRPSWDDPEXQDVXFFHV-VLyFRPSOHWDGHIjFLHVVHGLPHQWjULHVGHVGmiddotXQDIjFLHVb

OLPLWDGDDGRVSHWLWVWUDPVAgraveQVXQDIjFLHVc molt extensa

)LJ6HFFLyGHODOtQLD7GHO6RQ-

deig CE

30


1LYHOOamp(DTXHVWQLYHOOHVWUREDHVWqVSHUWRWDODSDUWEDL[DGHOWDO~VHQHO6RQGHLJamp(pVDGLUXQVP2

$OKRUDWDPEppVHOQLYHOODPEWUDPVPpVSRWHQWVTXHHQDOJXQVSXQWVDVVROHL[HOVFP(QHOVTXDGUHVL9HVYDQGRFXPHQWDU VHQJOHV IRUDWVGHSDO DOLQHDWVIRUPDWVSHUDFXPXODFLRQVGHFODVWHVSHWLWV(VWUREDYHQassentats i enterrats pel nivell CE14 i coberts en la seva

part superior per CE13 Tal com succeeix amb el nivell

amp(DTXHVWWDPEpSUHVHQWDXQDVXFFHVVLyFRPSOHWDGHOHVIjFLHVVHGLPHQWjULHVGHVGmiddotXQDbDPESRFDH[WHQVLyLsobretot una JAgraveQVDXQDFDSDEDVDOc

621(amp9(63$middot+shy7$7

$TXHVWVRQGHLJRFXSDXQWRWDOGHP2LHVORFDOLW]DDOD]RQDGHOYHVWtEXO(QXQWUHEDOODQWHULRUMDDYDQojUHPLQFLSLHQW LQIRUPDFLy DO UHVSHFWH 2PV et al 2010) La

potegravencia dels seus nivells acostuma a ser escassa despreacutes

drsquouna espessa crosta carbonatada es documenten una segrave-

ULH GmiddotHVWUXFWXUHV DQWUzSLTXHV LPEULFDGHV TXH SUHVHQWHQuna cronologia compresa entre el Neoliacutetic antic Cardial

AgraveQDOLqSRFDWDUGRUURPDQDLLQFO~VAgraveQVOmiddotDFWXDOLWDW

3HUWDQHQWDODIDVHPpVDQWLJDFRUUHVSRQHQXQWRWDOGHWUHVHVWUXFWXUHVGHFRPEXVWLyAgraveJVLGRVQLYHOOVGmiddotDERFDPHQW GH FHQGUHV WUHV HVWUDWV GmiddotRFXSDFLy XQGmiddotHOOVFRPSOHWDPHQWUXEDIHFWDWGXHVIRVVHVRJUDQVIR-

UDWVGHOSDOFLQFSHWLWVIRUDWVGHSDODVVRFLDWVDOD(VWUXF-WXUD GHampRPEXVWLy Q WUHV IRVVHVFRQWHQLGRU GLQV XQUHWDOOHOAtildeOLSVRwGDOLXQWRWDOGHIRUDWVGHSDOPpVGLVSHU-VRVSHOVQLYHOOVGmiddotRFXSDFLyYXLWGHPLGDJUDQ

(VWUXFWXUHVGHFRPEXVWLy(ampHVWUDFWDGHWUHVHV-tructures negatives totes elles en cubeta sense parament

exterior de blocs En dos dels casos (EC-4 i EC-8) es van

H[FDYDUGLUHFWDPHQWDODFURVWDSOLVWRFHQDPHQWUHTXHOmiddotDO-WUHIRJDU(ampHVYDH[FDYDUHQHOQLYHOOSOLVWRFqHVWqULOdrsquoargiles no carbonatades La EC-1 eacutes una estructura prou

SRWHQWDPESUREDEOHVUHXWLOLW]DFLRQVLDPEXQDHVWUXFWXUD-FLy FRPSOH[D UHWDOODW SHU XQ IRUDW GH SDO GH OD IDVH GHOURQ]HLQLFLDOD(amppVXQSHWLWIRJDUGHWHQGqQFLDFLU-FXODUHQYROWDWGmiddotXQHVWUDWUXEDIHFWDWTXHHOWDOODWDQJHQFLDO-ment de cronologia posterior no compta amb material

DUTXHROzJLFGLUHFWDPHQWDVVRFLDWSHUzVLHQHOVHVWUDWVTXHel cobreixen La EC-8 eacutes una estructura de tendegravencia irregu-

ODUVHPEODWUDFWDUVHGmiddotXQIRJDUUHQWDWMDTXHODGLVSRVLFLy

Fig 6 Planta de les ocupacions del neo-

liacutetic antic del Sondeig CV

31


GHODFRPEXVWLypVLUUHJXODULFRPSWDDPEHQWUDGHVGHJUD-YHWHVLVRUUHVTXHVHPEOHQUHEOLUSUREDEOHVFDXV

)RUDWVGHSDO)3QmiddotKLKDGHGRVWLSXVGLIHUHQWVHOVSHWLWVVLWXDWVDUHGyVGHOD(ampLHOVGHPLGDJUDQ(OVprimers (cinc) tenen unes dimensions drsquoentre 6 i 8 cm de

GLjPHWUHPj[LPLXQDSRWqQFLDTXHQRDVVROHL[HQFDSFDVels 10 cm tots ells de desenvolupament totalment verti-

FDO(OVDOWUHVYXLWGHOVTXDOVVLVSDUFLDOPHQWDOLQHDWVFRPSWHQDPEXQVGLjPHWUHVSURSHUVDOVFPLXQDSR-

WqQFLDPj[LPDGHFP)RVVHV)(VWUDFWDGHIRVVHVGHWHQGqQFLDFLUFXODU

(irregular) excavades en la crosta plistocena estegraveril

6middotKDQGHAgraveQLWFRPSHUWDQHQWVDOmiddotKRULW]yGHO1HROtWLFDQ-

WLFampDUGLDOAgraveQDOSHUHVWDUVHJHOODGHVSHUDOJXQHVXQLWDWVGHQHWHMDRGmiddotRFXSDFLy7HQHQXQHVGLPHQVLRQVGmiddotHQWUHFPLXQDSRWqQFLDVLPLODU(OVHXIDUFLPHQWSHUWDQHQSDUWDOVHVWUDWVVXSHULRUVTXHOHVVHJHOOHQSHUzWDPEpXQ LPSRUWDQW FRPSRQHQW GH VRUUHV L JUDYHWHV$TXHVWVIDFWRUVHQVIDQSURSRVDUXQDIXQFLyQRWDQWGHVLWJHVVLQyPpVDYLDWGHIRVVDFRQWHQLGRUSUREDEOHPHQWSHUVXEMHF-WDUKLYDVRVRSRWVHUFRPDJUDQVIRUDWVGHSDOGHWLSXVprincipalestructural

- Fosses-contenidor (FC) es tracta de tres petites

IRVVHV PROW MXQWHV H[FDYDGHV GLQV GmiddotXQ UHWDOO HOOLSVRwGDOGHTXDVLFPGHOODUJ$TXHVWHVHV WUREHQtocant a un gran bloc estructural del sondeig Colomera

9HVWtEXOSHUDTXHVWDUDyFUHLHPMXQWDPEOHVGLPHQVLRQVGH OHV HVWUXFWXUHV TXH HV WUDFWD GH FORWV RQ UHFRO]DUYDVRV FHUjPLFV8Q GmiddotHOOV HV WUREDYD DPRUWLW]DW DPEuna base de moliacute

(VWUDWVGmiddotRFXSDFLy LHVWUDWVGHQHWHMDDTXHVWVQL-YHOOVVyQHOVTXHSURSRUFLRQHQXQPDMRUQRPEUHGHPD-WHULDOVDUTXHROzJLFV(VWUDFWDGHERVVDGHVGHVHGLPHQWHQ OOHXJHUV UHWDOOV SHU VRWD OD FURVWD VXSHULRU TXH QRVXSHUHQJHQHUDOPHQWHOVFPGHSRWqQFLD1RIRUPHQJUDQVXQLWDWVVLQyPpVDYLDWHVWUDWVGmiddotH[WHQVLyOLPLWDGDsovint retallats per estrats similars de cronologies poste-

riors Es troben generalment associats a estructures de

FRPEXVWLySHUDTXHVWPRWLXLSHU ODVHYDFRPSRVLFLyDOJXQVGmiddotDTXHVWV HVWUDWV KDQ HVWDW FRQVLGHUDWV FRPHV-WUDWVGHQHWHMDGHIRJDUV(VWUDFWDGmiddot8(VGmiddotXQDSRWqQFLDirregular compostos sempre per una matriu heterogegravenia

IRUPDGDSHUVRUUHWHVLOOLPVDPEXQFRPSRQHQWGmiddotDUJL-les molt baix) amb presegravencia de pocs blocs i clastes

FHQWLPqWULFV DPE FODUV HVWLJPHV GH WHUPRDOWHUDFLyLrsquoalta presegravencia de carbons en alguns casos de mida

JUDQLVREUHWRWGHUHVWHV]RRDUTXHROzJLTXHVFUHPDGHVLFDOFLQDGHVVyQOHVFDUDFWHUtVWLTXHVGmiddotDTXHVWVQLYHOOV

ELS MATERIALS ARQUEOLOgraveGICS

(OSULPHUSUREOHPDTXHVmiddotKDGmiddotHVPHQWDUpVHOGHODFRQVWUXFFLyIRUPDFLyGHOGLSzVLWDUTXHROzJLFLODVHYDGLVSRVLFLy(QDTXHVWVHQWLWLVREUHWRWHQHOVQLYHOOVGHfumier HO SURSL PDWHULDO DUTXHROzJLF GRFXPHQWDW HQels nivells pot procedir del mateix lloc o pot procedir

GmiddotXQDHOLPLQDFLyGHUHVLGXVHQPXQWVGHIHPVLKHUEHVSURFHGHQWVGHGLIHUHQWV OORFVGH ODFDYLWDW(QDTXHVWVHJRQFDVHOVHOHPHQWVHVWUREDULHQHQSRVLFLyVHFXQ-

GjULDWRWLTXHin situHQHOPRPHQWGHODIRUPDFLyGHOQLYHOO (O IHW TXH F GHOV IUDJPHQWV GHOV QLYHOOVamp( SUHVHQWLQ WUDFHV GmiddotLPSUHJQDFLy GH VHGL-ment de fumierFODSHVGHVHGLPHQWFULVWDOAtildeOLW]DWDGKHULW

)LJ PDWJHVGHO6RQGHLJamp9]RQDGmiddotKjELWDW$9LVWDGH WUHVIRVVHVFRQWHQLGRUHQJDQ[DGHVDXQEORFHVWUXFWXUDO HOGH ODGUHWDHVWjVHJHOODWSHUXQPROtIUDJPHQWDW)3DPEXQYDVHVFODIDWD OmiddotLQWHULRUamp)RVVD DEDQVGHOV VHXEXLGDWJH$OLQHDFLyGHIRUDWVGHSDOHQSULPHUWHUPHIRJDUVLIRVVHVDODGUHWD

32


DOVIUDJPHQWVQRPpVGHPRVWUDTXHHOVHIHFWLXVHVWUR-

baven inserits en el sediment en el moment de la com-

EXVWLy5HVSHFWHDODIRUPDFLyGHOVQLYHOOVGHO1HROtWLFDQWLFGHO6RQGHLJamp9DTXHVWVUHVSRQHQDXQDDFWLYLWDWGLUHFWDVREUHHOVQLYHOOVDPEIDVHVGHQHWHMDDPRUWLW-]DFLy LFODXVXUDQDWXUDORDQWUzSLFDGHGLIHUHQWVHV-trats i retalls

(6$(6amp(5shy048(6

DUUHUDPHQWHVSUHVHQWjXQWUHEDOODPEOHVGDGHVFH-UjPLTXHV UHIHUHQWV D OHV FDPSDQHV 2PVmiddotHQojGmiddotDTXHOOPRPHQWHOVQLYHOOVGHO1HROtWLFantic del sondeig CE no srsquohan treballat intensivament i el

volum de material no ha augmentat substancialment En

FDQYL VmiddotKDQ SRWHQFLDW OHV IHLQHV DO VRQGHLJ amp9 L SHUDTXHVWPRWLXDOJXQHVGHOHVGDGHVKDQYDULDWVXEVWDQFLDO-PHQWHQDTXHVWGDUUHUVRQGHLJ

(OQLYHOOGHIUDJPHQWDFLyGHOPDWHULDOFHUjPLFpVPROWDOWHQHOVGRVVRQGHMRVWRWLTXHHQJHQHUDOHOVIUDJPHQWVVyQPDMRUVDOD]RQDGHOfumier En el Sondeig CV predo-

PLQHQHOVYDVRVPLWMDQVLSHWLWVPHQWUHTXHHQHO6RQGHLJamp(VyQPpVKDELWXDOVHOVYDVRVPLWMDQVJUDQVLJUDQV2PVHVPRUIRORJLHVGHOVYDVRVQRPRVWUHQGLIHUqQFLHVVXEVWDQFLDOVMDTXHHQHOVGRVFDVRVSUHGRPLQHQHOVYDVRVVLPSOHVRYRLGHVLVXEHVIqULFVLFRPSRVWRVDPEFROOGHVWD-FDWeV LOAtildeOXVWUDWLYDSHUz ODSUHVqQFLDPDMRUGHYDVRVGHSHUAgraveOFLOtQGULFUHFWLOLQLDOVRQGHLJamp($QLYHOOGHGHFRUD-FLRQVHVSHFtAgraveTXHVOHVGLIHUqQFLHVVyQSRFLPSRUWDQWVHQHOlapse complet malgrat aixograve la presegravencia de decoracions

ERTXLTXH L FDUGLDOV DPESHUFHQWDWJHVEDL[RVQRPpV pVGRFXPHQWDGDDOVRQGHLJamp93HU~OWLPFDOGHVWDFDUTXHQRsrsquohan documentat remuntatges directes o indirectes entre

YDVRV(QFRQFOXVLyHVSRWDAgraveUPDUTXH ODSUHVqQFLDGHPDWHULDOV FHUjPLFVDO6RQGHLJamp(

SRWFRUUHVSRQGUHDIDFWRUVGLUHFWHVUHFLSLHQWVSHUUHFROOLUaigua o abeurar animals recollir llet etc) o indirecte

DPXQWHJDPHQWMXQWDPEGmiddotDOWUHVHOHPHQWVSURFHGHQWVGHGLIHUHQWVSDUWVGHODFDYLWDW

ODSUHVqQFLDGHIUDJPHQWVPpVJUDQVDOVRQGHLJamp(SRWLQGLFDUQRPpVKDYHUVRIHUWPHQVSUREOHPHVGHWUDPSOLQJ

OHVGLIHUqQFLHVHQWUHOHVPLGHVGHOVYDVRVPRUIROR-

JLHVLHOSHUFHQWDWJHGHGHFRUDFLRQVHQWUHHOVVRQGHMRVWRWLTXHSDWHQWVQRVyQSURXVLJQLAgraveFDWLYHVSHUHVWDEOLUXQDFRPSOHPHQWDULHWDWHQWUHHOVjPELWV

3HUWDQWOHVUHVWHVFHUjPLTXHVGmiddotDTXHVWDIDVHQRSHU-PHWHQHVWDEOLUXQDUHODFLyGLUHFWDHQWUHHOVGRVVRQGHMRV

$1Ocirc675$Igrave7amp$

HVUHVWHVGRFXPHQWDGHVVyQPROWHVFDVVHV LQRSHU-PHWHQLQIHULUGDGHVHQWRUQODIXQFLRQDOLWDWGHFDGDjPELW~QLFDPHQWGHVWDFDODPDMRUSUHVqQFLDGmiddotHIHFWLXVDOD]RQDGmiddotHVWDEXODFLy 15 YHUV HO VRQGHLJ amp9 15 (OPpVUHPDUFDEOHpVTXHDODFRYDQRPpVDUULEHQOHVSDUWVWHUPLQDOVGH ODFDGHQDRSHUDWLYD SHUIRUDGRUVJUDWDGRUVOjPLQHVLOjPLQHVUHWRFDGHVQRHVGRFXPHQWHQQXFOLVQLSUjFWLFDPHQWUHVWHVGHWDOODDVFOHVRDVFOHVIUDJPHQWDGHV(OIHWGHWUDQVSRUWDUHOVHOHPHQWVMDFRQAgraveJXUDWVLDEDQGRQDWVSRVWHULRUPHQW D OD VHYD IUDJPHQWDFLy HV SRW UHODFLRQDUamb la inaccessibilitat de la cova i a priori amb curtes

HVWDGHVDODFRYDRDXQDUHGXwGDRFXSDFLyTXDQWDSREOD-FLyDSURFHGqQFLDGHODPDMRULDGmiddotHIHFWLXVOtWLFVHVFRU-UHVSRQDPEORFDOLW]DFLRQVSURSHUHVNPWUREDQWVHDOJXQVFDVRVHVSRUjGLFV15 SURFHGHQWVGHODYDOOGHlrsquoEbre (Mangado et al 2012)

)LJLPHQVLRQVGHOVIUDJPHQWVFHUjPLFVSHUVRQGHLJLFDUDFWH-UtVWLTXHVVLJQLAgraveFDWLYHVVHJRQVHOVRQGHLJ

33


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

amp9TXHSUHVHQWHQPpVDOWHUDFLRQVLPDUTXHV$L[zHVcontraposa amb les dades del sondeig CE on les restes

LGHQWLAgraveFDGHV VyQ PROW PDMRUV L SUHVHQWHQPHQVIUDFWXUDFLyLXQPHQRUQRPEUHGHPDUTXHVGHWDOOo de bullit

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


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


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


$$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

(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


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

F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO

6(53SW3UHKLVWzULD+LVWzULD$QWLJDL$UTXHRORJLD8QLYHUVLWDWGHDUFHORQD[DYLHURPVJPDLOFRP

PDQJDGRXEHGXPLUHLDSHGURJPDLOFRP

PDULDXEHURXEHGX

JUAN M LOacutePEZ-GARCIacuteA

Gruppo di Recerca di Paleobiologia e Preistoria

8QLYHUVLWjGL)HUUDUDOS]MPQXQLIHLW

PATRICIA MARTIN

JUAN I MORALES

ANNA RODRGIacuteGUEZ

3+(6Universitat Rovira i Virgili

SDWULPUJPDLOFRPMLJQDFLRPRUDOHVJPDLOFRPDQURGULJXH]FUX]JPDLOFRP

SUSANA MENDIELA

8QLWDWGmiddot$QWURSRORJLD)DFXOWDWGHLRORJLD8QLYHUVLWDWGHDUFHORQD

VXVDQDPHQGLHODJPDLOFRP

AgraveGATA RODRIacuteGUEZ-CINTAS

(3(SW3UHKLVWzULD+LVWzULD$QWLJDL$UTXHRORJLD8QLYHUVLWDWGHDUFHORQDDJDWDUFKRWPDLOFRP

NOTA

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

HOVWUHEDOOVGHFDPSDL[tFRPDWRWVHOVDUTXHzOHJVTXHIDQUHFHU-FDGHOMDFLPHQW3HU~OWLPKHPGmiddotDJUDLUOHVFRUUHFFLRQVLFRPHQ-

WDULVUHDOLW]DWVSHOVGRVFRUUHFWRUVDQzQLPV

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

$1(8ampamp26amp+$1)217$1$603(527-

7$9(5Euml6-06KHSKHUGVDQGNDUVW WKHXVHRIFDYHVDQGURFNVKHOWHUVLQWKH0HGLWHUUDQHDQUHJLRQduring the NeolithicRUOG$UFKDHRORJ 41 (2) 191-214

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


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

2KWWSG[GRLRUJ)($9($-$SOHFGHGRFXPHQWVDUTXHROzJLFVGHOHV

FRYHVGHO0RQWVHFLOOXUSURMHFFLyDOHVFRPDUTXHVLVHUUHVproperes 0HGLWHUUjQLD 12

38


$6ampETH-08(5amp$UFKLWHFWXUHHWIRQFWLRQQHPHQWGmiddotXQHPDLVRQFKDVVpHQHj5RFDGRXU7KpPLQHVRWDe ODPDLVRQDXYLOODJHmiddotKDELWDWQpROLWKLTXHGDQVOHV6XGGHla France et le Nord-Ouest meacutediterraneacuteen$HHFKLQJSeacuteneacutepart dirs) Marsella 89-98

21=shy(=0$5ampe13$5amp$8e(3=$552-(O)RUDWGHODampRQTXHWDSREODPHQWQHROtWLFLXVRVIXQHUDULVGHOULQPLOAtildeOHQQLHQHO3UHSLULHQHXGHOHLGD7ULEXQDGmiddot$UTXHRORJLD 2009 99-120

GUILAINE J MARTZLUFF M (1995) Les excavacions a la DOPDGHOD0DUJLQHGD Andorra

0$1$2025$(6-206)5(lt06Eacute1-

amp+(=($7255(0(VWXGLGHOHVUHVWHVOtWL-TXHVGHODampRYDampRORPHUDHQWUHLFDOamp$QjOL-VLDUTXHRSHWUROzJLFDGHOHVPDWqULHVSULPHUHVVLOtFLHVLOHVVHYHVSRVVLEOHVjUHHVGHFDSWDFLy$FWHVGHOampRQJUpVQWHU-national Xarxes al NeoliacuteticDUFHORQD

0(675(6-5e$SUR[LPDFLyDOmiddotHVWXGLGHOHVHV-WUDWqJLHVGmiddotRFXSDFLyGHOmiddot$OW3HQHGqVGXUDQWHO1HROtWLFIX ampROAtildeORTXLQWHUQDFLRQDOGmiddot$UTXHRORJLDGH3XLJFHUGj(VWDWGHODQYHVWLJDFLyVREUHHO1HROtWLFDampDWDOXQD3XLJFHUGji Andorra la Vella 85-88

025$5(172amp$92$0$571(=025(12-21-

=Eacute(=0$5ampe13($7255(ampKURQRVWUD-WLJUDSKRIWKH8SSHU3OHLVWRFHQHDQG+RORFHQHDUFKDHRORJLFDOVHTXHQFHLQampRYDUDQVRXWKHDVWHUQ3UH3UHQHHVEHULDQ3H-ninsula) -RXUQDORI4XDWHUQDU6FLHQFH 26 (6) 635-644

2KWWSG[GRLRUJMTV206)ampDUDFWHULW]DFLyWqFQLFDWLSROzJLFDLFURQROzJLFDGH

OHVFHUjPLTXHVGHO1HROtWLFDQWLFDODampRYDampRORPHUD3UHSL-rineu de Lleida) APL XXVII 51-80

206)$5$ETH$amp+$(50)217$1$60GARCIacuteA M S LOacutePEZ J MORALES J I NIEVAS

7525Igrave8(=$6(55$-62e$9(5e6-M (2008) La Cova Colomera (Sant Esteve de la Sarga

Lleida) una cueva-redil en el Prepirineo de Leacuterida Prime-

URVUHVXOWDGRVSHUVSHFWLYDVGHIXWXURActas del IV Con-JUHVR GHO 1HROtWLFR 3HQLQVXODU 0 6 +HUQiQGH] -$6ROHU-$ySH]HGV$ODFDQW

206)$5$ETH$ETH3(=$5amp$-0025$-

(6-3(52062eshymiddotDUTXHRORJLDprehistograverica a la Serra del Montsec (Prepirineu de Lleida)

GHVGHOVHJOHAgraveQVOmiddotDFWXDOSURMHFWHGHUHFHUFDRevista Gmiddot$UTXHRORJLDGH3RQHQW 19 29-50

206)3(520$5$ETH$ETH3(=$5ampIgrave$ -0025$(6-62e$(OSURMHFWHDUTXHR-

OzJLFDOD6HUUDGHO0RQWVHF3DOODUV-XVVj1RYHVGDGHVSHOFRQHL[HPHQWGHOQHROtWLFLHGDWGHOEURQ]HDO3UHSLULQHXGHLleida QampROAtildeORTXLGmiddot$UTXHRORJLDGmiddot2GqQ Odegraven 39-46

OMS F X PETIT M A MORALES J I GARCIacuteA M S (2012)

HSURFHVVXVGHQpROLWKLVDWLRQGDQV OHV3UpQpHVRULHQWDOHVOccupation du milieu culture mateacuterielle et chronologie Bu-lletin de la Socieacuteteacute Preacutehistorique Franccedilaise 109 (4) 651-670

3$$5e6025$6$025$5(OSURFHVRGHQHROL-WL]DFLyQHQORV3LULQHRV2ULHQWDOHV8QPRGHORGHFRQWLQXLGDGHQWUHORVFD]DGRUHVUHFROHFWRUHVQHROtWLFRVORVSULPHURVJUX-

pos agropastoriles 7UDEDMRVGH3UHKLVWRULD 54 (1) 121-141


PETIT M (eacuted) (1996) El proceacutes de neolititzacioacute a la Vall del Se-JUHDampRYDGHO3DUFR$OzVGHDODJXHU(VWXGLGHOHVocupacions humanes del Vegrave al II milmiddotlenni aCDUFHORQD

RAMOacuteN N (2006) DFHUiPLFDGHO1HROtWLFRDQWLJXRHQ$UDJyQ

=DUDJR]D52$1e6 -05$0ETH11 (O1HROtWLFR DQWLJXR HQ

$UDJyQKiELWDWWHUULWRULRZephyrus XLVIII 101-128

52-20$52lt2-$5525$5ampIgrave$0$57Igrave1(=($5Eacute17(-(25amp$5amp86$+$5ampIgrave$$=2$= - 6(60$ - (8567$1 0 $RVFDPLQRVGHO1HROtWLFRXQSURHFWRGHLQYHVWL-JDFLyQHQHOYDOOHGHO(EUR$FWHVGHOampRQJUpVQWHUQDWLR-nal Xarxes al NeoliacuteticDUFHORQD

ROVIRA J CURA M (1992) Observacions sobre alguns materials

del Neoliacutetic Antic i Antic Avanccedilat del Prepirineu de Lleida IX ampROAtildeORTXLQWHUQDFLRQDOGmiddot$UTXHRORJLDGH3XLJFHUGj(VWDWGHODLQYHVWLJDFLyGHO1HROtWLFDampDWDOXQD3XLJFHUGj

7+5$87e((amp+1$ 8QKDELWDW HQJURWWH DX1pROLWKLTXHDQFLHQOHVFDEDQHVGHDXPHGH5RQ]H2UJ-

nac Ardegraveche) HODPDLVRQDXYLOODJHmiddotKDELWDWQpROLWKL-que dans les Sud de la France et le Nord-Ouest meacutediterra-neacuteen$HHFKLQJ6pQpSDUWGLU0DUVHOOD

875$ 3 (SLSDOHROtWLFRV 1HROtWLFRV GHO 9DOOH GHOEbro El paisaje en el Neoliacutetico Mediterraacuteneo (DGDO-HUQDEpX0DUWtHGV9DOqQFLD

UTRILLA P (2012) Caminos para el neoliacutetico aragoneacutes la apor-

WDFLyQGHOUDGLRFDUERQRGHODUWHUXSHVWUHActes del Con-JUpVQWHUQDWLRQDODU[HVDO1HROtWLFDUFHORQD

875$325(1=2-$(289623(1$0amp$lt8623(QWHUUDPLHQWRPDVFXOLQRHQIRVDFXELHU-to de cantos rodados en el Neoliacutetico antiguo de la Cueva de

Chaves9ampRQJUHVRGHO1HROtWLFR3HQLQVXODU06+HUQiQ-

GH]-$6ROHU-$ySH]HGV$ODFDQWUTRILLA P MAZO C (2007) La pentildea de las Forcas de Graus

+XHVFD 8Q DVHQWDPLHQWR UHLWHUDGR GHVGH HO 0DJGDOH-niense hasta el Neoliacutetico antiguo Salduie 7 9-37

9(5$6amp2amp HSyVLWRV QDWXUDOHV GH FXHYD DOWHUDGRVHVWXGLRPLFURVHGLPHQWROyJLFRGHDFXPXODFLRQHVSURGXFL-GDVHQHOQHROtWLFRYDOHQFLDQRSRUODHVWDEXODFLyQGHRYLFi-pridos ampXDWHUQDULRHUPRUIRORJtD 15 (3-4) 8594

9(5Euml6 -0$8e($1(8ampamp85-$amp+6)amp$55$1amp+2$amp(5shy$(3ETH672)217$-

NALS M MORAL S RODRIacuteGUEZ A VAQUERO

M (2008) Los niveles neoliacuteticos de la cueva del Mirador

6LHUUDGH$WDSXHUFDXUJRVQXHYRVGDWRVVREUHODLPSODQ-

WDFLyQHOGHVDUUROORGHODHFRQRPtDDJURSHFXDULDHQODVXE-

meseta norte 9ampRQJUHVRGHO1HROtWLFR3HQLQVXODU (M S

+HUQiQGH]-$6ROHU-$ySH]HGV$ODFDQW

26


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








(c 30-50)














28


































29





















SHUXQDIjFLHVJ





deig CE

30






















31
























32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































27








(c 30-50)














28


































29





















SHUXQDIjFLHVJ





deig CE

30






















31
























32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































28


































29





















SHUXQDIjFLHVJ





deig CE

30






















31
























32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































29





















SHUXQDIjFLHVJ





deig CE

30






















31
























32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































30






















31
























32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































31
























32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































32





(6$(6amp(5shy048(6


















33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































33





















34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































34





USOS DE LrsquoESPAI































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































35







vells CE12 i CE14










36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































36



















CONCLUSIONS







37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































37





F XAVIER OMS

XAVIER MANGADO

MIREIA PEDRO

MARIA YUBERO



PDULDXEHURXEHGX




PATRICIA MARTIN

JUAN I MORALES




SUSANA MENDIELA





NOTA





BIBLIOGRAFIA



$1(8ampamp26amp+$1)217$1$603(527-

















38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































38





0$1$2025$(6-206)5(lt06Eacute1-



025$5(172amp$92$0$571(=025(12-21-








206)$5$ETH$ETH3(=$5amp$-0025$-


































h (p l n - core.ac.uk · gdwdfly prvwuduld xq odsvh Àqdo gh od idvh dtxt dqdolw]dgd )lj 0dwhuldov...

Documents