Arid
DOI10.18172/cig.1999
Paleoenvironmental reconstruction of the last glacial cycle in the continental Iberia: the Canizar de Villarquemado sequence (Teruel)
Gonzalez-Samperiz, P.; Garcia-Prieto, E.; Aranbarri, J.; Valero-Garces, B. L.; Moreno, A.; Gil-Romera, G.; Sevilla-Callejo, M.; Santos, L.; Morellon, M.; Mata, P.; Andrade, A.; Carrion, J. S.
通讯作者Gonzalez-Samperiz, P
来源期刊CUADERNOS DE INVESTIGACION GEOGRAFICA
ISSN0211-6820
EISSN1697-9540
出版年2013
卷号39期号:1页码:49-76
英文摘要El Canizar de Villarquemado sequence (North-eastern Iberian Peninsula) stands as an exceptional palaeoenvironmental record for the last 130 000 years. The preliminary multidisciplinary study carried out so far include pollen and sedimentological analyses, comprising geochemical, X ray fluorescence (XRF), mineralogical, organic and inorganic content (TOC/TIC) analyses. The chronological model has been established combining AMS 14C on the first 20 m of sediment and OSL methods on the remaining 54 m to the bottom. The sedimentary sequence is essentially formed by alternating facies of peatbogs and wetlands with those of distal alluvial fan deposits and others of carbonate lake. The results currently obtained support relatively humid conditions at El Caizar de Villarquemado during a likely MIS6-MIS5 period, as errors linked to the age model prevent us to guarantee precisely the period boundaries. Despite indications of humidity, the regional vegetation variations during the MIS6-MIS5 period, essentially represented by Juniperus, were constrained by the intense continentality of the area, resulting in unexpected pollen assemblages for an interglacial period as the Eemian. The most arid phase of the sequence is registered during the MIS3, as shown by the available sedimentological and palynological results, while the MIS2 presents greater local and regional variability as proved by the sedimentary facies and aquatics and the other pollen spectra, respectively. The Holocene presents an abrupt onset regarding palaeohydrology while terrestrial vegetation, dominated by pine instead than Juniperus as in the sequence's bottom, show a resilient response as these are well adapted communities to extreme continentality. The later development of both, evergreen and marcescent Quercus, together with the presence of pine woodland, indicate very different climatic conditions between the MIS5 and MIS1 interglacial periods.
英文关键词hydrological variability continentality resilience aridity Eemian Holocene last glacial cycle
类型Article
语种西班牙语
开放获取类型DOAJ Gold, Green Accepted
收录类别ESCI
WOS记录号WOS:000421530300003
WOS关键词MILLENNIAL-SCALE VARIABILITY ; PLEISTOCENE POLLEN SEQUENCE ; GRANDE DI MONTICCHIO ; INTERGLACIAL CONDITIONS ; ENVIRONMENTAL-CHANGES ; NORTHEASTERN SPAIN ; DANSGAARD-OESCHGER ; SOUTHERN EUROPE ; CARIHUELA CAVE ; CENTRAL SECTOR
WOS类目Geography, Physical
WOS研究方向Physical Geography
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/330524
作者单位[Gonzalez-Samperiz, P.; Garcia-Prieto, E.; Aranbarri, J.; Valero-Garces, B. L.; Moreno, A.; Gil-Romera, G.; Sevilla-Callejo, M.] CSIC, Inst Pirenaico Ecol, Av Montanana 1005, Zaragoza 50059, Spain
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Gonzalez-Samperiz, P.,Garcia-Prieto, E.,Aranbarri, J.,et al. Paleoenvironmental reconstruction of the last glacial cycle in the continental Iberia: the Canizar de Villarquemado sequence (Teruel)[J],2013,39(1):49-76.
APA Gonzalez-Samperiz, P..,Garcia-Prieto, E..,Aranbarri, J..,Valero-Garces, B. L..,Moreno, A..,...&Carrion, J. S..(2013).Paleoenvironmental reconstruction of the last glacial cycle in the continental Iberia: the Canizar de Villarquemado sequence (Teruel).CUADERNOS DE INVESTIGACION GEOGRAFICA,39(1),49-76.
MLA Gonzalez-Samperiz, P.,et al."Paleoenvironmental reconstruction of the last glacial cycle in the continental Iberia: the Canizar de Villarquemado sequence (Teruel)".CUADERNOS DE INVESTIGACION GEOGRAFICA 39.1(2013):49-76.
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