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DOI | 10.1016/j.palaeo.2020.109630 |
Tuff fingerprinting and correlations between OGCP cores and outcrops for Pre-Bed I and Beds I/II at Olduvai Gorge; Tanzania | |
McHenry L.J.; Stanistreet I.G.; Stollhofen H.; Njau J.K.; Toth N.; Schick K. | |
发表日期 | 2020 |
ISSN | 0031-0182 |
卷号 | 548 |
英文摘要 | Sediment cores retrieved from the Pleistocene Olduvai Basin by the Olduvai Gorge Coring Project (OGCP) provide a high resolution record of tuffs and other volcaniclastic deposits, together with a lacustrine sedimentary record full of paleoenvironmental indicators. Correlating tuffs between the cores and outcrops at Olduvai, where these tuffs are identified at paleoanthropologically important sites, is critical for applying the new paleoenvironmental data to the conditions under which hominins lived. Tuffs and other volcaniclastic deposits from three cores were analyzed for mineral assemblages and glass and mineral major element compositions (feldspar, augite, hornblende, titanomagnetite, and glass where possible) to compare to published geochemical fingerprint data, based on marker tuffs from outcrop equivalents at Olduvai Gorge. In combination with stratigraphic position, these mineralogical and geochemical data were used to correlate between the cores and outcrops, providing direct temporal tie-lines between the cores and sites of paleoanthropological interest. Direct correlations are most certain for Olduvai Bed I, where all major tuff markers from outcrop are identified for one or more of the three core sites, and for the upper part of the underlying Ngorongoro Formation, which includes the Coarse Feldspar Crystal Tuff (CFCT) and Naabi ignimbrites exposed in the oldest Pleistocene exposures of the Western Gorge. Also characterized were the mineral and glass compositions of tuffs and ignimbrites pre-dating the oldest exposed outcrop units, extending our record of explosive events from the Ngorongoro Volcano. While no specific correlations can be confirmed between individual Bed II tuffs in the cores and in outcrops, correlations are possible between the cores themselves (using newly identified tuff compositions), and some potential correlations (non-unique, based on individual mineral phases) between core and outcrop can be used in conjunction with other stratigraphic tools to help constrain the intervals in question. © 2020 Elsevier B.V. |
英文关键词 | East Africa; Geochemistry; Mineral assemblage; Pleistocene; Tephra; Tephrostratigraphy |
语种 | 英语 |
scopus关键词 | geochemical survey; lithostratigraphy; Olduvai event; outcrop; paleoenvironment; Pleistocene; tephra; tephrochronology; tuff; volcaniclastic deposit; Arusha [Tanzania]; Ngorongoro; Olduvai Gorge; Tanzania |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150518 |
作者单位 | Department of Geosciences, University of Wisconsin-Milwaukee, 3209 N. Maryland Ave., Milwaukee, WI 53211, United States; Dept. Earth, Ocean and Ecological Sciences, University of Liverpool, Brownlow Street, Liverpool, L69 3GP, United Kingdom; The Stone Age Institute, Bloomington, IN 47407-5097, United States; GeoZentrum Nordbayern, Friedrich-Alexander-University (FAU) Erlangen-Nürnberg, Schloßgarten 5, Erlangen, 91054, Germany; Department of Earth and Atmospheric Sciences, Indiana University, 1001 East 10th Street, Bloomington, IN 47405-1405, United States |
推荐引用方式 GB/T 7714 | McHenry L.J.,Stanistreet I.G.,Stollhofen H.,et al. Tuff fingerprinting and correlations between OGCP cores and outcrops for Pre-Bed I and Beds I/II at Olduvai Gorge; Tanzania[J],2020,548. |
APA | McHenry L.J.,Stanistreet I.G.,Stollhofen H.,Njau J.K.,Toth N.,&Schick K..(2020).Tuff fingerprinting and correlations between OGCP cores and outcrops for Pre-Bed I and Beds I/II at Olduvai Gorge; Tanzania.Palaeogeography, Palaeoclimatology, Palaeoecology,548. |
MLA | McHenry L.J.,et al."Tuff fingerprinting and correlations between OGCP cores and outcrops for Pre-Bed I and Beds I/II at Olduvai Gorge; Tanzania".Palaeogeography, Palaeoclimatology, Palaeoecology 548(2020). |
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