Tephrostratigraphy and depositional environment of young (

Erin N. DiMaggio, Ramon Arrowsmith, Christopher Campisano, Roy Johnson, Alan L. Deino, Mark Warren, Shimeles Fisseha, Andrew S. Cohen

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

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, 40Ar/39Ar age of 2.931 ± 0.017 Ma (1σ). 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.

Original languageEnglish (US)
Pages (from-to)234-250
Number of pages17
JournalJournal of African Earth Sciences
Volume112
DOIs
StatePublished - Dec 1 2015

Fingerprint

depositional environment
basin
valley
conglomerate
sedimentary rock
Pliocene
outcrop
volcanic eruption
drilling
sedimentation
young
sediment
project

Keywords

  • Afar depression
  • Hadar Formation
  • Hominin paleoenvironments
  • Pliocene
  • Stratigraphy
  • Tephrochronology

ASJC Scopus subject areas

  • Earth-Surface Processes
  • Geology

Cite this

Tephrostratigraphy and depositional environment of young (. / DiMaggio, Erin N.; Arrowsmith, Ramon; Campisano, Christopher; Johnson, Roy; Deino, Alan L.; Warren, Mark; Fisseha, Shimeles; Cohen, Andrew S.

In: Journal of African Earth Sciences, Vol. 112, 01.12.2015, p. 234-250.

Research output: Contribution to journalArticle

DiMaggio, Erin N. ; Arrowsmith, Ramon ; Campisano, Christopher ; Johnson, Roy ; Deino, Alan L. ; Warren, Mark ; Fisseha, Shimeles ; Cohen, Andrew S. / Tephrostratigraphy and depositional environment of young (. In: Journal of African Earth Sciences. 2015 ; Vol. 112. pp. 234-250.
@article{0e114d4a6ed2415fba4779a632a876a6,
title = "Tephrostratigraphy and depositional environment of young (",
abstract = "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, 40Ar/39Ar age of 2.931 ± 0.017 Ma (1σ). 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.",
keywords = "Afar depression, Hadar Formation, Hominin paleoenvironments, Pliocene, Stratigraphy, Tephrochronology",
author = "DiMaggio, {Erin N.} and Ramon Arrowsmith and Christopher Campisano and Roy Johnson and Deino, {Alan L.} and Mark Warren and Shimeles Fisseha and Cohen, {Andrew S.}",
year = "2015",
month = "12",
day = "1",
doi = "10.1016/j.jafrearsci.2015.09.018",
language = "English (US)",
volume = "112",
pages = "234--250",
journal = "Journal of African Earth Sciences",
issn = "1464-343X",
publisher = "Elsevier Limited",

}

TY - JOUR

T1 - Tephrostratigraphy and depositional environment of young (

AU - DiMaggio, Erin N.

AU - Arrowsmith, Ramon

AU - Campisano, Christopher

AU - Johnson, Roy

AU - Deino, Alan L.

AU - Warren, Mark

AU - Fisseha, Shimeles

AU - Cohen, Andrew S.

PY - 2015/12/1

Y1 - 2015/12/1

N2 - 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, 40Ar/39Ar age of 2.931 ± 0.017 Ma (1σ). 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.

AB - 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, 40Ar/39Ar age of 2.931 ± 0.017 Ma (1σ). 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.

KW - Afar depression

KW - Hadar Formation

KW - Hominin paleoenvironments

KW - Pliocene

KW - Stratigraphy

KW - Tephrochronology

UR - http://www.scopus.com/inward/record.url?scp=84943748041&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84943748041&partnerID=8YFLogxK

U2 - 10.1016/j.jafrearsci.2015.09.018

DO - 10.1016/j.jafrearsci.2015.09.018

M3 - Article

AN - SCOPUS:84943748041

VL - 112

SP - 234

EP - 250

JO - Journal of African Earth Sciences

JF - Journal of African Earth Sciences

SN - 1464-343X

ER -