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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Isotopic paleoecology (delta C-13) from mammals from IUIU/BA and paleoenvironmental reconstruction (delta C-13, delta O-18) for the Brazilian intertropical region through the late Pleistocene
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Isotopic paleoecology (delta C-13) from mammals from IUIU/BA and paleoenvironmental reconstruction (delta C-13, delta O-18) for the Brazilian intertropical region through the late Pleistocene

机译:来自Iuuu / Ba和古环境重建(Delta C-13,Delta O-18)的来自哺乳动物的同位素古生态(Delta C-13)通过晚期渗透官能

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Stable isotopes of carbon and oxygen of fossil specimens are widely used for paleoecological and paleoenvironmental inferences, and there has been an effort to better understand the isotopic paleoecology and chronology of herbivores that inhabited the Brazilian Intertropical Region during the late Quaternary. In the present work, new radiocarbon datings and carbon and oxygen isotopes data for Eremotherium laurillardi, Notiomastodon platensis, Tapirus terrestris, Tayassu pecan, and Mazama gouazoubira are presented, from specimens that lived on Iuiu county (Toca Fria and Jatoba caves), state of Bahia, in the Brazilian Intertropical Region. E. laurillardi was dated as of similar to 32 ka BP, representing the oldest direct dating for this species in the Brazilian Intertropical Region, while N. platensis was dated as of similar to 25 ka BP. Fossils of the extant species T. pecan, M. gouazoubira, and T. terrestris presented radiocarbon ages of similar to 23 ka BP, similar to 21 ka BP, and similar to 15 ka BP, respectively, showing that some of these species lived in Iuiu during the Last Glacial Maximum. According to our analyses, T. terrestris was the only specialist (delta C-13 = -11.0 parts per thousand; p(i)C(3) = 0.76; B-A = 0.49), whereas the remaining taxa were generalists mixed-feeders (delta C-13 = -1.3 to -10.0 parts per thousand; p(i)C(3) = 0.24 to 0.69; B-A > 0.58). The paleoenvironment reconstruction in Iuiu and other localities in BIR, during similar to 32 ka BP to similar to 15 ka BP, allow us to suggest that the dry arboreal to open Savanna habitats (rich in grass and shrubs) were the most common environment. (C) 2020 Elsevier Ltd. All rights reserved.
机译:碳和氧气的稳定同位素是化石标本的广泛应用于古生态和古环境推论,并且曾经努力更好地了解在第四纪后期居住的巴西闭管会区域的食草动物同位素古生态和年表。在目前的工作中,展示了新的Raurillardi,Notiomastodon Platensis,Tapirus Terress,Tayassu Pecan和Mazama Gouazoubira的新的Radiocarbon和碳和氧同位素数据,从居住在Iuu县(Toca Fria和Jatoba Caves)的标本,巴伊亚,在巴西闭圈地区。 E. Laurillardi的日期为类似于32 KA BP,代表巴西闭管区域中最古老的直接约会,而N.Platensis与25kP相似。现存物种T.Pecan,M.Gouazoubira和T. Terrestris的化石呈现与23ka BP相似的无碳芸香铜,同样类似于21 kA BP,类似于15 kA BP,显示出这些物种中的一些物种居住IUIU在最后的冰川最大值。根据我们的分析,T. Terrestris是唯一的专家(Delta C-13 = -11.0份千分之一; P(i)C(3)= 0.76; Ba = 0.49),而剩下的分类群是通用混合饲养者( Delta C-13 = -1.3至-10.0份每千份; P(i)C(3)= 0.24至0.69; Ba> 0.58)。 IUIU和BIR中其他地方的古环境重建,在类似于32 KA BP的情况下,与15 kA BP类似,让我们建议打开大草原栖息地(富含草和灌木)是最常见的环境。 (c)2020 elestvier有限公司保留所有权利。

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