Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica
Abstract Postel Nunatak in the Patuxent Range has been previously mapped as Nelson Limestone but there was no biostratigraphic support for that interpretation until now. We confirm that limestone exposures at Postel Nunatak are at least partly correlated with the Nelson Limestone of the Neptune Rang...
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crcambridgeupr:10.1017/s0954102017000396 2024-03-03T08:37:57+00:00 Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica Evans, Kevin Ray McKenna, Lawrence W. Lieberman, Bruce S. Weichert, Wesley Donald Macleod, Kenneth G. 2017 http://dx.doi.org/10.1017/s0954102017000396 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102017000396 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Antarctic Science volume 30, issue 1, page 29-43 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2017 crcambridgeupr https://doi.org/10.1017/s0954102017000396 2024-02-08T08:47:14Z Abstract Postel Nunatak in the Patuxent Range has been previously mapped as Nelson Limestone but there was no biostratigraphic support for that interpretation until now. We confirm that limestone exposures at Postel Nunatak are at least partly correlated with the Nelson Limestone of the Neptune Range, 160 km north-east, and are not correlative with the lower Cambrian Schneider Hills Limestone of the Argentina Range. Upper beds have yielded the trilobites Suludella? davnii Palmer & Gatehouse, 1972 and Solenopleura pruina Palmer & Gatehouse, 1972, which provide a basis for assignment to Cambrian Series 3 (late middle Cambrian), within the Drumian or lower Guzhangian stages. Limestone beds were deposited in a shallow marine setting, ranging from supratidal to lagoonal facies with rare subtidal intervals. These settings contrast with deeper water facies of the Neptune Range. Despite limitations in sampling density, isotopic analysis indicates that a greater than +2.5‰ shift in δ 13 C is consistent with δ 13 C trends documented for the Drumian Stage. Because the upper and lower contacts at Postel Nunatak are covered by snow and ice, the relationship with rocks mapped as the Patuxent Formation in the Patuxent Range remains uncertain, but part of it may belong to the Precambrian Hannah Ridge Formation. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Cambridge University Press Argentina Hannah ENVELOPE(-60.613,-60.613,-62.654,-62.654) Neptune Range ENVELOPE(-53.000,-53.000,-84.000,-84.000) Hannah Ridge ENVELOPE(-54.992,-54.992,-83.605,-83.605) Patuxent Range ENVELOPE(-64.500,-64.500,-84.716,-84.716) Argentina Range ENVELOPE(-42.172,-42.172,-82.362,-82.362) Schneider Hills ENVELOPE(-42.701,-42.701,-82.571,-82.571) Postel Nunatak ENVELOPE(-67.766,-67.766,-84.883,-84.883) Antarctic Science 30 1 29 43 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
spellingShingle |
Geology Ecology, Evolution, Behavior and Systematics Oceanography Evans, Kevin Ray McKenna, Lawrence W. Lieberman, Bruce S. Weichert, Wesley Donald Macleod, Kenneth G. Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica |
topic_facet |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
description |
Abstract Postel Nunatak in the Patuxent Range has been previously mapped as Nelson Limestone but there was no biostratigraphic support for that interpretation until now. We confirm that limestone exposures at Postel Nunatak are at least partly correlated with the Nelson Limestone of the Neptune Range, 160 km north-east, and are not correlative with the lower Cambrian Schneider Hills Limestone of the Argentina Range. Upper beds have yielded the trilobites Suludella? davnii Palmer & Gatehouse, 1972 and Solenopleura pruina Palmer & Gatehouse, 1972, which provide a basis for assignment to Cambrian Series 3 (late middle Cambrian), within the Drumian or lower Guzhangian stages. Limestone beds were deposited in a shallow marine setting, ranging from supratidal to lagoonal facies with rare subtidal intervals. These settings contrast with deeper water facies of the Neptune Range. Despite limitations in sampling density, isotopic analysis indicates that a greater than +2.5‰ shift in δ 13 C is consistent with δ 13 C trends documented for the Drumian Stage. Because the upper and lower contacts at Postel Nunatak are covered by snow and ice, the relationship with rocks mapped as the Patuxent Formation in the Patuxent Range remains uncertain, but part of it may belong to the Precambrian Hannah Ridge Formation. |
format |
Article in Journal/Newspaper |
author |
Evans, Kevin Ray McKenna, Lawrence W. Lieberman, Bruce S. Weichert, Wesley Donald Macleod, Kenneth G. |
author_facet |
Evans, Kevin Ray McKenna, Lawrence W. Lieberman, Bruce S. Weichert, Wesley Donald Macleod, Kenneth G. |
author_sort |
Evans, Kevin Ray |
title |
Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica |
title_short |
Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica |
title_full |
Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica |
title_fullStr |
Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica |
title_full_unstemmed |
Geology of the Nelson Limestone, Postel Nunatak, Patuxent Range, Antarctica |
title_sort |
geology of the nelson limestone, postel nunatak, patuxent range, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
2017 |
url |
http://dx.doi.org/10.1017/s0954102017000396 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102017000396 |
long_lat |
ENVELOPE(-60.613,-60.613,-62.654,-62.654) ENVELOPE(-53.000,-53.000,-84.000,-84.000) ENVELOPE(-54.992,-54.992,-83.605,-83.605) ENVELOPE(-64.500,-64.500,-84.716,-84.716) ENVELOPE(-42.172,-42.172,-82.362,-82.362) ENVELOPE(-42.701,-42.701,-82.571,-82.571) ENVELOPE(-67.766,-67.766,-84.883,-84.883) |
geographic |
Argentina Hannah Neptune Range Hannah Ridge Patuxent Range Argentina Range Schneider Hills Postel Nunatak |
geographic_facet |
Argentina Hannah Neptune Range Hannah Ridge Patuxent Range Argentina Range Schneider Hills Postel Nunatak |
genre |
Antarc* Antarctic Science Antarctica |
genre_facet |
Antarc* Antarctic Science Antarctica |
op_source |
Antarctic Science volume 30, issue 1, page 29-43 ISSN 0954-1020 1365-2079 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1017/s0954102017000396 |
container_title |
Antarctic Science |
container_volume |
30 |
container_issue |
1 |
container_start_page |
29 |
op_container_end_page |
43 |
_version_ |
1792503105475051520 |