John Diemer

Datos Biográficos

ID	6042536
NOMBRE	John Diemer
NOMBRES	John
APELLIDO	Diemer
FIRMA	DIEMER J
AFILIACIONES	University of North Carolina at Charlotte
ORCID	0000-0002-0697-5648
VERIFICADO	Sí
TOTAL DE OBRAS	4
TOTAL DE CITAS	0
TOTAL COMO AUTOR	4
TOTAL COMO EDITOR	0
PRIMER AÑO DE PUBLICACIÓN	1995
AÑO MÁS RECIENTE DE PUBLICACIÓN	2013
ÍNDICE H	0

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 AccessBradley G Johnson, Gonzalo Jiménez‐moreno et al.ARTICLEThe Holocene2013Referencias: 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 AccessBradley G Johnson, Martha Cary Eppes et al.ARTICLEQuaternary Research2011
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 AccessBradley G Johnson, Martha Cary Eppes et al.ARTICLEJournal of Maps2010
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…
Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie
Michael Collie, John Diemer et al.ARTICLETransactions of the American…1995
Michael Collie, John Diemer, Roderick Impey Murchison, George Gordon of Birnie, Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie, Transactions of the American Philosophical Society, New Series, Vol. 85, No. 3 (1995), pp. i-xxix+1-263

Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie
Michael Collie, John Diemer et al.ARTICLETransactions of the American…1995
Michael Collie, John Diemer, Roderick Impey Murchison, George Gordon of Birnie, Murchison in Moray a Geologist on Home Ground with the Correspondence of Roderick Impey Murchison and the Rev. Dr. George Gordon of Birnie, Transactions of the American Philosophical Society, New Series, Vol. 85, No. 3 (1995), pp. i-xxix+1-263
Surficial Geologic Map of the Upper Conejos River Drainage, Southeastern San Juan Mountains, Southern Colorado, USA
Open AccessBradley G Johnson, Martha Cary Eppes et al.ARTICLEJournal of Maps2010
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 AccessBradley G Johnson, Martha Cary Eppes et al.ARTICLEQuaternary Research2011
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 AccessBradley G Johnson, Gonzalo Jiménez‐moreno et al.ARTICLEThe Holocene2013Referencias: 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…