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Estella B Leopold

Biographic Data

ID2138839
NAMEEstella B Leopold
GIVEN NAMESEstella B
FAMILY NAMELeopold
SIGNATURELEOPOLD E B
AFFILIATIONSUniversity of Washington
VERIFIEDNo
TOTAL WORKS9
TOTAL CITATIONS12
WORKS AS AUTHOR9
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1964
LATEST PUBLICATION YEAR2016
H-INDEX1
  • Postglacial vegetation history of Orcas Island, northwestern Washington

    Open Access•Estella B Leopold, Peter W Dunwiddie et al.•ARTICLE•Quaternary Research•2016

    The revegetation of islands following retreat of Pleistocene glaciers is of great biogeographical interest. The San Juan Islands, Washington, feature regionally distinctive xerophytic plant communities, yet their vegetation history, as it relates to past climate and sea level, is poorly known. We describe a 13,700-year-old pollen record from Killebrew Lake Fen and compare the vegetation reconstruction with others from the region. The data suggest…

  • Introducing the Scientific Consensus on Maintaining Humanity's Life Support Systems in the 21st Century

    Open Access•Anthony D Barnosky, Jennifer H Brown et al.•ARTICLE•The Anthropocene Review•2014•Cited by: 12•References: 79

    The Anthropocene is recognized (though not yet formally defined) as the time when human impacts are widespread on Earth. While some of the impacts are essential to supporting large human populations and can be sustainable in the long run, others can irretrievably damage the life support systems upon which the global society has come to depend, or spark rapid changes to which societies cannot adapt fast enough. Among these dangerous trends are inc…

  • Saved in Time

    Estella B Leopold, Herbert W Meyer•BOOK•Saved in time•2012

  • Plio-Pleistocene climatic transition and the lifting of the Teton Range, Wyoming

    Open Access•Estella B Leopold, Gengwu Liu et al.•ARTICLE•Quaternary Research•2007

    Fine-grained lacustrine, riverine and ash-fall sediments of the Shooting Iron Formation, whose late Pliocene age is established by Blancan gastropods and vertebrates, yield a pollen flora that is essentially similar in composition to the modern pollen rain in the Jackson Hole area. The Pliocene assemblage suggests a climate like that of the Jackson valley and foothills today. These spectra also resemble a Pliocene pollen flora from Yellowstone Pa…

  • Holocene Relative Sea Level Changes along the Seattle Fault at Restoration Point, Washington

    Open Access•Brian L Sherrod, Robert C Bucknam et al.•ARTICLE•Quaternary Research•2000

    At a marsh on the hanging wall of the Seattle fault, fossil brackish water diatom and plant seed assemblages show that the marsh lay near sea level between ∼7500 and 1000 cal yr B.P. This marsh is uniquely situated for recording environmental changes associated with past earthquakes on the Seattle fault. Since 7500 cal yr B.P., changes in fossil diatoms and seeds record several rapid environmental changes. In the earliest of these, brackish condi…

  • Late-Glacial and Early Holocene Sea-Level Fluctuations in the Central Puget Lowland, Washington, Inferred from Lake Sediments

    Open Access•Karl Anundsen, Sally Abella et al.•ARTICLE•Quaternary Research•1994

    Analyses of sediments, diatoms, and pollen in a 12.65-m-long sediment core taken from Lake Carpenter in the central Puget Lowland, Washington, provide detailed information regarding the history of deglaciation and late-glacial/early Holocene sea-level changes. The lake outlet, now 8.2 m above sea level, has been lowered 1-1.5 m by postglacial erosion. The lithology and pollen record suggest that no lengthy hiatuses in sedimentation have occurred.…

  • A long pollen sequence of Neogene age, Alaska range

    Open Access•Estella B Leopold, Gengwu Liu•ARTICLE•Quaternary International•1994

  • Appendix II

    Open Access•Estella B Leopold, Joe Ben Wheat•ARTICLE•Memoirs of the Society for…•1972

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama

    Watson Hiner Monroe, Richard Edwards Bergenback et al.•REPORT•1964

    In 1954 four core holes were drilled in the pre-Selma Cretaceous strata of the Alabama Coastal Plain in order to get unweathered samples within a few miles of the outcrops. During the next few years several specialists studied the cores, and their reports are published as consecutive parts of this bulletin. Watson H. Monroe, who spent many years studying the Coastal Plain strata in Alabama and Mississippi, conceived and supervised the drilling an…

  • Introducing the Scientific Consensus on Maintaining Humanity's Life Support Systems in the 21st Century

    Open Access•Anthony D Barnosky, Jennifer H Brown et al.•ARTICLE•The Anthropocene Review•2014•Cited by: 12•References: 79

    The Anthropocene is recognized (though not yet formally defined) as the time when human impacts are widespread on Earth. While some of the impacts are essential to supporting large human populations and can be sustainable in the long run, others can irretrievably damage the life support systems upon which the global society has come to depend, or spark rapid changes to which societies cannot adapt fast enough. Among these dangerous trends are inc…

  • Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama

    Watson Hiner Monroe, Richard Edwards Bergenback et al.•REPORT•1964

    In 1954 four core holes were drilled in the pre-Selma Cretaceous strata of the Alabama Coastal Plain in order to get unweathered samples within a few miles of the outcrops. During the next few years several specialists studied the cores, and their reports are published as consecutive parts of this bulletin. Watson H. Monroe, who spent many years studying the Coastal Plain strata in Alabama and Mississippi, conceived and supervised the drilling an…

  • Appendix II

    Open Access•Estella B Leopold, Joe Ben Wheat•ARTICLE•Memoirs of the Society for…•1972

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Late-Glacial and Early Holocene Sea-Level Fluctuations in the Central Puget Lowland, Washington, Inferred from Lake Sediments

    Open Access•Karl Anundsen, Sally Abella et al.•ARTICLE•Quaternary Research•1994

    Analyses of sediments, diatoms, and pollen in a 12.65-m-long sediment core taken from Lake Carpenter in the central Puget Lowland, Washington, provide detailed information regarding the history of deglaciation and late-glacial/early Holocene sea-level changes. The lake outlet, now 8.2 m above sea level, has been lowered 1-1.5 m by postglacial erosion. The lithology and pollen record suggest that no lengthy hiatuses in sedimentation have occurred.…

  • A long pollen sequence of Neogene age, Alaska range

    Open Access•Estella B Leopold, Gengwu Liu•ARTICLE•Quaternary International•1994

  • Holocene Relative Sea Level Changes along the Seattle Fault at Restoration Point, Washington

    Open Access•Brian L Sherrod, Robert C Bucknam et al.•ARTICLE•Quaternary Research•2000

    At a marsh on the hanging wall of the Seattle fault, fossil brackish water diatom and plant seed assemblages show that the marsh lay near sea level between ∼7500 and 1000 cal yr B.P. This marsh is uniquely situated for recording environmental changes associated with past earthquakes on the Seattle fault. Since 7500 cal yr B.P., changes in fossil diatoms and seeds record several rapid environmental changes. In the earliest of these, brackish condi…

  • Plio-Pleistocene climatic transition and the lifting of the Teton Range, Wyoming

    Open Access•Estella B Leopold, Gengwu Liu et al.•ARTICLE•Quaternary Research•2007

    Fine-grained lacustrine, riverine and ash-fall sediments of the Shooting Iron Formation, whose late Pliocene age is established by Blancan gastropods and vertebrates, yield a pollen flora that is essentially similar in composition to the modern pollen rain in the Jackson Hole area. The Pliocene assemblage suggests a climate like that of the Jackson valley and foothills today. These spectra also resemble a Pliocene pollen flora from Yellowstone Pa…

  • Saved in Time

    Estella B Leopold, Herbert W Meyer•BOOK•Saved in time•2012

  • Introducing the Scientific Consensus on Maintaining Humanity's Life Support Systems in the 21st Century

    Open Access•Anthony D Barnosky, Jennifer H Brown et al.•ARTICLE•The Anthropocene Review•2014•Cited by: 12•References: 79

    The Anthropocene is recognized (though not yet formally defined) as the time when human impacts are widespread on Earth. While some of the impacts are essential to supporting large human populations and can be sustainable in the long run, others can irretrievably damage the life support systems upon which the global society has come to depend, or spark rapid changes to which societies cannot adapt fast enough. Among these dangerous trends are inc…

  • Postglacial vegetation history of Orcas Island, northwestern Washington

    Open Access•Estella B Leopold, Peter W Dunwiddie et al.•ARTICLE•Quaternary Research•2016

    The revegetation of islands following retreat of Pleistocene glaciers is of great biogeographical interest. The San Juan Islands, Washington, feature regionally distinctive xerophytic plant communities, yet their vegetation history, as it relates to past climate and sea level, is poorly known. We describe a 13,700-year-old pollen record from Killebrew Lake Fen and compare the vegetation reconstruction with others from the region. The data suggest…

Geology and Paleoclimatology Research (6 works) · Ecology (5 works) · Geology (5 works) · Pollen (5 works) · Geography (4 works) · Paleontology (4 works) · Biology (3 works) · Botany, Ecology, and Taxonomy Studies (3 works) · Ecology (3 works) · Geology (3 works)

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