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The long paleoenvironmental sequence of Santimamine (Bizkaia,Spain): 20,000 years of small mammal record from the latest Late Pleistocene to the middle Holocene

机译:Santimamine(西班牙Bizkaia)的古环境序列:从最新的晚更新世到中全新世的20,000年小型哺乳动物记录

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摘要

The cave of Santimamine (Kortezubi, Bizkaia, Spain), on the southern slopes of the Erenozar Mountain (Urdaibai biosphere reserve), is one of the most famous prehistoric localities of the Cantabrian range. Between 2004 and 2006, a test trench revealed a 6 m-deep stratigraphic sequence in the inner vestibule of the cave covering ~20,000 years, from the latest Late Pleistocene (MIS 2) to the middle Holocene (MIS 1). It comprises six chrono-cultural units: lower, middle and upper Magdalenian, Azilian, Neolithic, and Chalcolithic/Bronze Age, plus seven lower purely palaeontological levels. More than 47,000 micro-vertebrate elements (including mammals, birds, reptiles, amphibians and fishes) were recovered, of which 1587 were identified to the genus and/or species levels. Of these, small mammals were used for paleoenvironmental reconstruction since they are very sensitive to climatic conditions and their distributions over time, measured in terms of relative abundance, serve as reliable proxies of habitat and climatic change. The reconstruction of Santimamine past environments based on small mammals roughly coincides with other proxies, such as the amphibian/reptile, large mammal/bird, palynological, and cryoclastic records on the local scale; other paleoenvironmental reconstructions from north Iberia on the regional scale; and the oxygen isotopic curve of an ice core from central Greenland on the global scale. All Magdalenian levels from Santimamine were deposited during the Oldest Dryas, a mostly cold and humid period including the Heinrich event 1. Small mammalian, palynological and cryoclastic evidence likely document the shift from the cold Younger Dryas to the beginning of the Holocene Climatic Optimum during Azilian times. The uppermost level, deposited during a moderate re-opening of the landscape at the Subboreal, slightly postdates the Holocene Cooling Event 3.
机译:Santimamine洞穴(Kortezubi,Bizkaia,西班牙)位于Erenozar山(Urdaibai生物圈保护区)的南坡上,是坎塔布连山脉最著名的史前地区之一。在2004年至2006年之间,一条测试沟槽揭示了从最近的晚更新世(MIS 2)到中全新世(MIS 1)约2万年的洞穴内部前庭深达6 m的地层层序。它由六个年代文化单位组成:下,中,上马格达林时代,阿兹利亚时代,新石器时代和中石器时代/青铜时代,以及七个较低的纯古生物学水平。回收了47,000多种微脊椎动物(包括哺乳动物,鸟类,爬行动物,两栖动物和鱼类),其中1587种在属和/或物种水平上得到了确认。其中,小型哺乳动物被用于古环境重建,因为它们对气候条件非常敏感,并且它们的时间分布(以相对丰度衡量)可以作为栖息地和气候变化的可靠代表。 Santimamine基于小型哺乳动物过去环境的重建与其他代理大致重合,例如两栖动物/爬行动物,大型哺乳动物/鸟类,孢粉学和当地的破冰记录;伊比利亚北部地区范围内的其他古环境重建;和格陵兰中部冰芯在全球范围内的氧同位素曲线。 Santimamine的所有Magdalenian含量都是在最古老的树as(包括Heinrich事件1)在内的最寒冷和潮湿的时期沉积的。哺乳动物,孢粉和冷碎屑的小证据可能记录了在Azilian时期从寒冷的年轻树Dry到全新世气候最佳时期的开始。次。最适度的沉积是在Subboreal的景观重新开放期间沉积的,略晚于全新世冷却事件3。

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  • 来源
    《Quaternary International》 |2014年第7期|62-75|共14页
  • 作者单位

    Universidad del Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Estratigrafia y Paleontologia, Apartado 644, E-48080 Bilbao,Spain,Universidad del Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Estratigrafia y Paleontologia, Sarriena s, 48940 Leioa, Bizkaia, Spain;

    Universidad del Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Estratigrafia y Paleontologia, Apartado 644, E-48080 Bilbao,Spain;

    Universidad del Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Estratigrafia y Paleontologia, Apartado 644, E-48080 Bilbao,Spain;

    UMR 7209-UMR 7149, CNRS Departement Ecologie et Gestion de la Biodiversite (EGB), MNHN Batiment d'Anatomie Comparee CP55,55 rue Buffon, 75005 Paris, France;

    AGIRI Arkeologia Kultura Elkartea, 208 Postakutxa, 48300 Gernika-Lumo, Spain;

    AGIRI Arkeologia Kultura Elkartea, 208 Postakutxa, 48300 Gernika-Lumo, Spain;

    Universidad de Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Mineralogia y Petrologia, Apartado 644, E-48080 Bilbao, Spain;

    Universidad de Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Mineralogia y Petrologia, Apartado 644, E-48080 Bilbao, Spain;

    Universidad de Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Mineralogia y Petrologia, Apartado 644, E-48080 Bilbao, Spain;

    Universidad del Pais Vasco UPV-EHU, Facultad de Ciencia y Tecnologia, Departamento de Estratigrafia y Paleontologia, Apartado 644, E-48080 Bilbao,Spain;

    Socedad de Ciencias Aranzadi, Zorroagagaina 11, 20014 Donostia-San Sebastian, Spain;

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