Tephrostratigraphy and depositional environment of young (<2.94 Ma) Hadar Formation deposits at Ledi-Geraru, Afar, Ethiopia

被引:5
|
作者
DiMaggio, Erin N. [1 ]
Arrowsmith, J. Ramon [2 ]
Campisano, Christopher J. [3 ]
Johnson, Roy [4 ]
Deino, Alan L. [5 ]
Warren, Mark [6 ]
Fisseha, Shimeles [7 ]
Cohen, Andrew S. [4 ]
机构
[1] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA
[2] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA
[3] Arizona State Univ, Sch Human Evolut & Social Change, Inst Human Origins, Tempe, AZ 85287 USA
[4] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
[5] Berkeley Geochronol Ctr, Berkeley, CA 94709 USA
[6] Conoco Phillips, Houston, TX 77079 USA
[7] Univ Addis Ababa, Inst Geophys Space Sci & Astron, Addis Ababa, Ethiopia
基金
美国国家科学基金会;
关键词
Afar depression; Hadar Formation; Pliocene; Tephrochronology; Stratigraphy; Hominin paleoenvironments; PLIOCENE HOMINIDS; AFRICAN CLIMATE; TRIPLE JUNCTION; MIDDLE AWASH; STONE TOOLS; EARLY HOMO; GONA; PLIOPLEISTOCENE; RIFT; EVOLUTION;
D O I
10.1016/j.jafrearsci.2015.09.018
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Pliocene Hadar Formation, exposed throughout the lower Awash Valley, Ethiopia, chronicles the evolution and paleoenvironmental context of early hominins. Deposition of the Hadar Formation continued until at least 2.94 Ma, but what transpired in the Hadar Basin after this time remains poorly documented due to an erosional event that truncated the formation throughout much of the valley. Here we present geologic mapping and stratigraphic analysis of a 26 m-thick section of sedimentary rocks and tephras exposed in the Ledi-Geraru project area in the region of Gulfaytu. The section contains Hadar Formation strata younger than 2.94 Ma, and sediments that we interpret are Busidima Formation in age, <2.7 Ma. We use this record to place additional constraints on depositional environments and the tectonic and paleogeomorphic history of the region. The lower similar to 20 m of section contains lacustrine deposits that conformably overly a 2.94 Ma marker bed (BKT-2U) that previously served as the uppermost dated tephra in the Hadar Formation. We identified seven post-BKT-2U tephras; three were analyzed for glass chemistry, and one yielded an 40Ar/39Ar age of 2.931 +/- 0.017 Ma (1 sigma). Based on these analyses, the newly mapped deposits at Gulfaytu extend the top of the Hadar Formation, representing ca. 20 kyr of post-BKT-2 sedimentation. The Hadar Basin remained depositional following the BKT-2 eruptions, and paleolake Hadar was present at Gulfaytu at this time. An erosional surface marked by a conglomerate truncates the Hadar strata suggesting that the Gulfaytu region was also was influenced by significant changes to basin architecture well-documented elsewhere in the lower Awash Valley. In addition, geophysical models suggest that central Ledi Geraru hosts a thick subsurface lacustrine sedimentary record within the Hadar Basin. The results of this paper provide the outcrop and near surface characterization for the Hominin Sites and Paleolakes Drilling Project (HSPDP) effort at Gulfaytu. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:234 / 250
页数:17
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