Cited by 171Geology and Paleoclimatology ResearchMarine and environmental studiesSoil and Environmental Studies

Nile Delta vegetation response to Holocene climate variability

Bernhardt, Christopher E., Horton, Benjamin P., Stanley, Jean-Daniel·2012·Geology

Abstract

Research Article| July 01, 2012 Nile Delta vegetation response to Holocene climate variability Christopher E. Bernhardt; Christopher E. Bernhardt * 1U.S. Geological Survey, 926A National Center, Reston, Virginia 20192, USA2Sea Level Research, Department of Earth and Environmental Science, University of Pennsylvania, 240 South 33rd Street, Hayden Hall, Philadelphia, Pennsylvania 19104, USA *E-mail: cbernhardt@usgs.gov. Search for other works by this author on: GSW Google Scholar Benjamin P. Horton; Benjamin P. Horton 2Sea Level Research, Department of Earth and Environmental Science, University of Pennsylvania, 240 South 33rd Street, Hayden Hall, Philadelphia, Pennsylvania 19104, USA Search for other works by this author on: GSW Google Scholar Jean-Daniel Stanley Jean-Daniel Stanley 3Geoarchaeology Program, Department of Paleobiology, E-205 NMNH, Smithsonian Institution, Washington, D.C. 20013-7012, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Christopher E. Bernhardt * 1U.S. Geological Survey, 926A National Center, Reston, Virginia 20192, USA2Sea Level Research, Department of Earth and Environmental Science, University of Pennsylvania, 240 South 33rd Street, Hayden Hall, Philadelphia, Pennsylvania 19104, USA Benjamin P. Horton 2Sea Level Research, Department of Earth and Environmental Science, University of Pennsylvania, 240 South 33rd Street, Hayden Hall, Philadelphia, Pennsylvania 19104, USA Jean-Daniel Stanley 3Geoarchaeol…

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Crossref · 10.1130/g33012.1

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  • The final century of the fourth millennium BC was a particularly dry period.

    “In the final century of the fourth millennium BC, during a particularly dry period (Bernhardt et al. 2012)”

    From The Egyptian Predynastic and State Formation (2016) · cites this paper as Bernhardt et al. 2012

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Authors
Bernhardt, C. E., Horton, B. P., & Stanley, J.-D.
Affiliations
  • United States Geological Survey (US)
  • University of Pennsylvania (US)
  • Smithsonian Institution (US)
Corresponding author
Bernhardt, Christopher E.
Venue
Geology
Published
2012-07
Volume
40
Issue
7
Pages
615-618
ISSN
  • 0091-7613 (ISSN-L)
  • 1943-2682
OpenAlex
W2021101742
Cited by
171
References
0
Citations by year
2026: 16 · 2025: 8 · 2024: 10 · 2023: 37 · 2022: 9 · 2021: 9 · 2020: 5 · 2019: 7 · 2018: 11 · 2017: 5 · 2016: 17 · 2015: 12 · 2014: 12 · 2013: 9 · 2012: 4
FWCI
8.08
Type
journal article
Language
en
Open access
closed
Locations
Geology (publishedVersion)
Funders
  • University of Pennsylvania
  • U.S. Geological Survey
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil and Environmental Studies
Keywords
Nile Delta, Holocene climate variability, vegetation history, paleoclimate, paleoecology, paleohydrology, paleoceanography, Holocene, vegetation dynamics, sea-level change, paleosols

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