Vegetation and climate record from Abric Romaní (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)

Demet Biltekin; Francesc Burjachs; Josep Vallverdú; Warren D. Sharp; Regina Mertz-Kraus; M. Gema Chacón; Palmira Saladié; James L. Bischoff; Eudald Carbonell

doi:10.1016/j.quascirev.2019.07.035

Vegetation and climate record from Abric Romaní (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)

Demet Biltekin^*
, Francesc Burjachs
, Josep Vallverdú
, Warren D. Sharp
, Regina Mertz-Kraus
, M. Gema Chacón
, Palmira Saladié
, James L. Bischoff
, Eudald Carbonell

^*Bu çalışma için yazışmadan sorumlu yazar

Institut Catala de Paleoecologia Humana i Evolucio Social (IPHES)
ICREA
Universidad Rovira i Virgili
Berkeley Geochronology Center
Johannes Gutenberg University Mainz

Araştırma çıktısı: Dergi yayını › Makale › Hakem

14 Atıf (Scopus)

Özet

This study addresses the pollen record of Abric Romaní archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of Artemisia steppes during the second part of the MIS 5a indicates that the degree of continentality can be related to the low winter temperatures and precipitation. During MIS 4, a colder and dryer climate enabled the development of open vegetation (dominated by Artemisia with Poaceae and other Asteraceae) around the study site.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	154-164
Sayfa sayısı	11
Dergi	Quaternary Science Reviews
Hacim	220
DOI'lar	https://doi.org/10.1016/j.quascirev.2019.07.035
Yayın durumu	Yayınlandı - 15 Eyl 2019
Harici olarak yayınlandı	Evet

Bibliyografik not

Publisher Copyright:
© 2019 Elsevier Ltd

Finansman

D. Biltekin has been supported by a postdoctoral research grant from the Scientific and Technological Research Council of Turkey (TUBITAK) and the research was supported by the Government of Catalonia (2009 SGR 813) and TUBITAK . We would like to thank the editor José S. Carrion and three anonymous reviewers for their constructive comments and useful recommendations that helped improve the quality of the paper.

Finansörler	Finansör numarası
TUBITAK
Generalitat de Catalunya	2009 SGR 813
Türkiye Bilimsel ve Teknolojik Araştirma Kurumu

Belgeye Erişim

10.1016/j.quascirev.2019.07.035

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

@article{63a31e957c714498983b001c93035620,

title = "Vegetation and climate record from Abric Roman{\'i} (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)",

abstract = "This study addresses the pollen record of Abric Roman{\'i} archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of Artemisia steppes during the second part of the MIS 5a indicates that the degree of continentality can be related to the low winter temperatures and precipitation. During MIS 4, a colder and dryer climate enabled the development of open vegetation (dominated by Artemisia with Poaceae and other Asteraceae) around the study site.",

keywords = "NE Iberian Peninsula, Palaeoclimatology, Palaeovegetation, Pollen analysis, Tufas",

author = "Demet Biltekin and Francesc Burjachs and Josep Vallverd{\'u} and Sharp, \{Warren D.\} and Regina Mertz-Kraus and Chac{\'o}n, \{M. Gema\} and Palmira Saladi{\'e} and Bischoff, \{James L.\} and Eudald Carbonell",

note = "Publisher Copyright: {\textcopyright} 2019 Elsevier Ltd",

year = "2019",

month = sep,

day = "15",

doi = "10.1016/j.quascirev.2019.07.035",

language = "English",

volume = "220",

pages = "154--164",

journal = "Quaternary Science Reviews",

issn = "0277-3791",

publisher = "Elsevier Ltd",

}

TY - JOUR

T1 - Vegetation and climate record from Abric Romaní (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)

AU - Biltekin, Demet

AU - Burjachs, Francesc

AU - Vallverdú, Josep

AU - Sharp, Warren D.

AU - Mertz-Kraus, Regina

AU - Chacón, M. Gema

AU - Saladié, Palmira

AU - Bischoff, James L.

AU - Carbonell, Eudald

PY - 2019/9/15

Y1 - 2019/9/15

N2 - This study addresses the pollen record of Abric Romaní archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of Artemisia steppes during the second part of the MIS 5a indicates that the degree of continentality can be related to the low winter temperatures and precipitation. During MIS 4, a colder and dryer climate enabled the development of open vegetation (dominated by Artemisia with Poaceae and other Asteraceae) around the study site.

AB - This study addresses the pollen record of Abric Romaní archaeological site and the climate evolution of the last interglacial and glacial stadials in the Iberian Peninsula. The new pollen record spans the interval from 110,000 to 55,000 years ago. In general, the glacial/stadial vegetation is characterized by a steppe and herbaceous communities indicating dry and cold climatic conditions, whereas the vegetation optimum of past interglacials can be described as pine-oaks with mediterranean forest indicating milder and moister climatic conditions. During the first half of the MIS 5a and the MIS 5c, the region was warmer, which is characterized by temperate forests. However, the existence of Artemisia steppes during the second part of the MIS 5a indicates that the degree of continentality can be related to the low winter temperatures and precipitation. During MIS 4, a colder and dryer climate enabled the development of open vegetation (dominated by Artemisia with Poaceae and other Asteraceae) around the study site.

KW - NE Iberian Peninsula

KW - Palaeoclimatology

KW - Palaeovegetation

KW - Pollen analysis

KW - Tufas

UR - https://www.scopus.com/pages/publications/85069920682

U2 - 10.1016/j.quascirev.2019.07.035

DO - 10.1016/j.quascirev.2019.07.035

M3 - Article

AN - SCOPUS:85069920682

SN - 0277-3791

VL - 220

SP - 154

EP - 164

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

ER -

Vegetation and climate record from Abric Romaní (Capellades, northeast Iberia) during the Upper Pleistocene (MIS 5d−3)

Özet

Bibliyografik not

Finansman

Belgeye Erişim

Diğer Dosyalar ve Linkler

Parmak izi

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