Radiometric, isotopic, and petrographic evidence of changing interglacials over the past 550,000 years from six stalagmites from the Serra do Courel in the Cordillera Cantábrica of northwestern Spain

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• 作者：L. Bruce Railsback^a ; ^{rlsbk@gly.uga.edu} ; Fuyuan Liang^b ; Juan Ramó ; n Vidal-Roman&iacute ; ^c ; Katelynn Blanche Garrett^a ; Rachel C. Sellers^a ; ¹ ; Marcos Vaqueiro-Rodr&iacute ; guez^c ; Aurora Grandal-d'Anglade^c ; Hai Cheng^d ; ^e ; R. Lawrence Edwards^e
• 关键词：Interglacials ; Stalagmites ; Spain ; Palaeoclimate ; Eemian ; Quaternary
• 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
• 出版年：2017
• 出版时间：15 January 2017
• 年：2017
• 卷：466
• 期：Complete
• 页码：137-152
• 全文大小：3308 K
• 卷排序：466

文摘

Six stalagmites deposited in interglacial stages (MIS 1, 5, 7, 13) but not glacials. Stalagmites are most effectively a record of wet versus dry. During interglacials, drier conditions when warmer and wetter when cooler. Stalagmite records support pollen-based records of Eemian and MIS 5c climate. Drier during coldest glacial and warmest interglacial times; wetter in intermediate.