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Michael J C Walker

Dados Biográficos

ID5601980
NOMEMichael J C Walker
PRENOMESMichael J C
SOBRENOMEWalker
ASSINATURAWALKER M J C
VERIFICADONão
TOTAL DE OBRAS3
TOTAL DE CITAÇÕES9
TOTAL COMO AUTOR3
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2000
ANO MAIS RECENTE DE PUBLICAÇÃO2010
ÍNDICE H1
  • Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma

    Open Access•Philip L Gibbard, Martin J Head et al.•ARTICLE•Journal of Quaternary Science•2010

    In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) formally ratified a proposal by the International Commission on Stratigraphy to lower the base of the Quaternary System/Period to the Global Stratotype Section and Point (GSSP) of the Gelasian Stage/Age at Monte San Nicola, Sicily, Italy. The Gelasian until then had been the uppermost stage of the Pliocene Series/Epoch. The base of the Gelasian correspo…

  • Implications for the Dating of Wisconsinan (Weichselian) Late-Glacial Events of Systematic Radiocarbon Age Differences between Terrestrial Plant Macrofossils from a Site in SW Ireland

    Open Access•Chris Turney, Chris S M Turney et al.•ARTICLE•Quaternary Research•2000

    AMS radiocarbon dates were obtained from Salix herbacea leaves, Carex seeds, and bulk organic detritus from a lake sediment profile of Wisconsinan (Weichselian) Lateglacial age in SW Ireland. There is a systematic age difference between the dated series from the two types of macrofossils, with ages obtained from Salix herbacea leaves being 900 to 1500 14 C years younger than those obtained from Carex seeds. The latter tend to be more in accord wi…

  • Radiocarbon Dating the Last Glacial-Interglacial Transition (Ca. 14–9 14 C Ka Bp) in Terrestrial and Marine Records

    Open Access•J John Lowe, Michael J C Walker•ARTICLE•Radiocarbon•2000•Citada por: 9•Referências: 81

    The publication during the 1990s of Greenland ice-core records spanning the transition from the Last Cold Stage to the present interglacial (ca. 14–9 14 C ka BP) presented new challenges to scientists working on marine and terrestrial sequences from this important time interval. In particular, there is now an overriding imperative to increase the levels of precision by which events during this period can be dated and correlated. We review some of…

  • Radiocarbon Dating the Last Glacial-Interglacial Transition (Ca. 14–9 14 C Ka Bp) in Terrestrial and Marine Records

    Open Access•J John Lowe, Michael J C Walker•ARTICLE•Radiocarbon•2000•Citada por: 9•Referências: 81

    The publication during the 1990s of Greenland ice-core records spanning the transition from the Last Cold Stage to the present interglacial (ca. 14–9 14 C ka BP) presented new challenges to scientists working on marine and terrestrial sequences from this important time interval. In particular, there is now an overriding imperative to increase the levels of precision by which events during this period can be dated and correlated. We review some of…

  • Implications for the Dating of Wisconsinan (Weichselian) Late-Glacial Events of Systematic Radiocarbon Age Differences between Terrestrial Plant Macrofossils from a Site in SW Ireland

    Open Access•Chris Turney, Chris S M Turney et al.•ARTICLE•Quaternary Research•2000

    AMS radiocarbon dates were obtained from Salix herbacea leaves, Carex seeds, and bulk organic detritus from a lake sediment profile of Wisconsinan (Weichselian) Lateglacial age in SW Ireland. There is a systematic age difference between the dated series from the two types of macrofossils, with ages obtained from Salix herbacea leaves being 900 to 1500 14 C years younger than those obtained from Carex seeds. The latter tend to be more in accord wi…

  • Radiocarbon Dating the Last Glacial-Interglacial Transition (Ca. 14–9 14 C Ka Bp) in Terrestrial and Marine Records

    Open Access•J John Lowe, Michael J C Walker•ARTICLE•Radiocarbon•2000•Citada por: 9•Referências: 81

    The publication during the 1990s of Greenland ice-core records spanning the transition from the Last Cold Stage to the present interglacial (ca. 14–9 14 C ka BP) presented new challenges to scientists working on marine and terrestrial sequences from this important time interval. In particular, there is now an overriding imperative to increase the levels of precision by which events during this period can be dated and correlated. We review some of…

  • Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma

    Open Access•Philip L Gibbard, Martin J Head et al.•ARTICLE•Journal of Quaternary Science•2010

    In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) formally ratified a proposal by the International Commission on Stratigraphy to lower the base of the Quaternary System/Period to the Global Stratotype Section and Point (GSSP) of the Gelasian Stage/Age at Monte San Nicola, Sicily, Italy. The Gelasian until then had been the uppermost stage of the Pliocene Series/Epoch. The base of the Gelasian correspo…

Geology and Paleoclimatology Research (3 obras) · Pleistocene-Era Hominins and Archaeology (3 obras) · Geography (2 obras) · Geology (2 obras) · Holocene (2 obras) · Interglacial (2 obras) · Paleontology (2 obras) · Physical geography (2 obras) · Quaternary (2 obras) · Radiocarbon dating (2 obras)

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