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John A Diemer

Dados Biográficos

ID8538764
NOMEJohn A Diemer
PRENOMESJohn A
SOBRENOMEDiemer
ASSINATURADIEMER J A
AFILIAÇÕESUniversity of North Carolina-Charlotte, USA
VERIFICADONão
TOTAL DE OBRAS3
TOTAL DE CITAÇÕES0
TOTAL COMO AUTOR3
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2010
ANO MAIS RECENTE DE PUBLICAÇÃO2013
ÍNDICE H0
  • A multiproxy record of postglacial climate variability from a shallowing, 12-m deep sub-alpine bog in the southeastern San Juan Mountains of Colorado, USA

    Open Access•Bradley G Johnson, Gonzalo Jiménez‐moreno et al.•ARTICLE•The Holocene•2013•Referências: 10

    Pollen assemblages, diatom assemblages, and sedimentology, from Cumbres Bog in the southeastern San Juan Mountains of Colorado, provide a record of climate and environmental change since the end of the last glacial maximum (LGM). Cumbres Bog is unusually deep (basal sediments extend 12 m below the surface) for its altitude (~3050 m a.s.l.) and we extracted 7 m core of continuous sediment below ~5 m of water and peat. The resulting record provides…

  • Post-glacial landscape response to climate variability in the southeastern San Juan Mountains of Colorado, USA

    Open Access•Bradley G Johnson, Martha Cary Eppes et al.•ARTICLE•Quaternary Research•2011

    Geomorphic mapping in the upper Conejos River Valley of the San Juan Mountains has shown that three distinct periods of aggradation have occurred since the end of the last glacial maximum (LGM). The first occurred during the Pleistocene–Holocene transition (~ 12.5–9.5 ka) and is interpreted as paraglacial landscape response to deglaciation after the LGM. Evidence of the second period of aggradation is limited but indicates a small pulse of sedime…

  • Surficial Geologic Map of the Upper Conejos River Drainage, Southeastern San Juan Mountains, Southern Colorado, USA

    Open Access•Bradley G Johnson, Martha Cary Eppes et al.•ARTICLE•Journal of Maps•2010

    Please click here to download the map associated with this article. During the Last Glacial Maximum (LGM), the San Juan Mountains of southern Colorado, USA were covered by one of the largest ice caps in North America. The deposits formed subsequent to LGM retreat provide a record of the interaction between post-LGM climate change and late Quaternary landscape evolution. In order to determine the role of post-LGM climate change in alpine landscape…

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  • Surficial Geologic Map of the Upper Conejos River Drainage, Southeastern San Juan Mountains, Southern Colorado, USA

    Open Access•Bradley G Johnson, Martha Cary Eppes et al.•ARTICLE•Journal of Maps•2010

    Please click here to download the map associated with this article. During the Last Glacial Maximum (LGM), the San Juan Mountains of southern Colorado, USA were covered by one of the largest ice caps in North America. The deposits formed subsequent to LGM retreat provide a record of the interaction between post-LGM climate change and late Quaternary landscape evolution. In order to determine the role of post-LGM climate change in alpine landscape…

  • Post-glacial landscape response to climate variability in the southeastern San Juan Mountains of Colorado, USA

    Open Access•Bradley G Johnson, Martha Cary Eppes et al.•ARTICLE•Quaternary Research•2011

    Geomorphic mapping in the upper Conejos River Valley of the San Juan Mountains has shown that three distinct periods of aggradation have occurred since the end of the last glacial maximum (LGM). The first occurred during the Pleistocene–Holocene transition (~ 12.5–9.5 ka) and is interpreted as paraglacial landscape response to deglaciation after the LGM. Evidence of the second period of aggradation is limited but indicates a small pulse of sedime…

  • A multiproxy record of postglacial climate variability from a shallowing, 12-m deep sub-alpine bog in the southeastern San Juan Mountains of Colorado, USA

    Open Access•Bradley G Johnson, Gonzalo Jiménez‐moreno et al.•ARTICLE•The Holocene•2013•Referências: 10

    Pollen assemblages, diatom assemblages, and sedimentology, from Cumbres Bog in the southeastern San Juan Mountains of Colorado, provide a record of climate and environmental change since the end of the last glacial maximum (LGM). Cumbres Bog is unusually deep (basal sediments extend 12 m below the surface) for its altitude (~3050 m a.s.l.) and we extracted 7 m core of continuous sediment below ~5 m of water and peat. The resulting record provides…

Geography (3 obras) · Geology and Paleoclimatology Research (3 obras) · Glacial period (3 obras) · Holocene (3 obras) · Physical geography (3 obras) · Climate change (2 obras) · Cryospheric studies and observations (2 obras) · Geology (2 obras) · Geomorphology (2 obras) · Landslides and related hazards (2 obras)

Ethnos_APP • Projeto Open Source • Licença MIT • Frontend v2.0.0 • Privacidade e Cookies • Documentação da API: api.ethnos.app/docs • Código da API: GitHub • DOI: 10.5281/zenodo.17049435 • Código do Frontend: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae