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坦桑尼亚奥杜威峡谷中中更新世第二期地层的古鸟类生态学以及奥杜威旧石器时代-阿舍利石器工业过渡时期的环境背景。

The paleoecology of Pleistocene birds from Middle Bed II, at Olduvai Gorge, Tanzania, and the environmental context of the Oldowan-Acheulean transition.

机构信息

Hagerman Fossil Beds National Monument, National Park Service, 221 North State Street, PO Box 570, Hagerman, ID 83332, USA.

Department of Anthropology, Colorado State University, 1787 Campus Delivery, Fort Collins, CO 80523, USA.

出版信息

J Hum Evol. 2018 Jul;120:32-47. doi: 10.1016/j.jhevol.2017.11.003. Epub 2018 Feb 17.

DOI:10.1016/j.jhevol.2017.11.003
PMID:29458978
Abstract

Fossil bird data (community composition and taphonomic profiles) are used here to infer the environmental context of the Oldowan-Acheulean transitional period at Olduvai Gorge, Tanzania. This is the first comprehensive report on the Middle Bed II avifauna and includes fossils excavated by the Olduvai Geochronology and Archaeology Project (OGAP) and recently rediscovered fossils collected by Mary Leakey. Crane, ibis, darter, owl, raptor, crow, and vulture are reported from Bed II for the first time. The presence of these taxa, absent earlier in this Bed, point to a general opening and drying of the landscape with grassland and open woodland expansion. Taxa associated with dense, emergent wetland vegetation, such as dabbling ducks and rails, are uncommon and less diverse than earlier in Bed II. This suggests more mature wetlands with clearer waters. Cormorants continue to be common, but are less diverse. Cormorants and other roosting taxa provide evidence of trees in the area. Compared to lowermost Bed II, the Middle to Upper Bed II landscape is interpreted here as more open and drier (but not necessarily more arid), with matured wetlands, scattered trees, and a greater expansion of grasslands.

摘要

本文利用古鸟类数据(群落组成和埋藏学特征)来推断坦桑尼亚奥杜威峡谷旧石器时代中期至晚期过渡时期的环境背景。这是对中 II 层鸟类群首次进行的全面报告,包括由奥杜威地质年代学和考古项目(OGAP)发掘的化石和玛丽·利基最近重新发现的化石。II 层首次报道了鹤、朱鹭、鱼狗、猫头鹰、猛禽、乌鸦和秃鹫。这些分类群在该地层早期不存在,表明景观总体上变得开阔和干燥,草原和开阔林地扩展。与密集、湿地植被相关的分类群,如涉禽和秧鸡,不太常见,也不如 II 层早期多样化。这表明湿地更成熟,水质更清澈。鸬鹚仍然很常见,但种类较少。鸬鹚和其他栖息类群为该地区有树木提供了证据。与下 II 层相比,中上层 II 层的景观被解释为更加开阔和干燥(但不一定更干旱),湿地成熟,树木散落,草原进一步扩展。

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Soil and plant phytoliths from the mosaics at Oldupai Gorge (Tanzania).来自奥杜威峡谷(坦桑尼亚)镶嵌区域的土壤和植物硅酸体。
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