Cretaceous marine invertebrates: A geochemical perspective.
A diagenetic evaluation was performed on marine fossil shell material from Cretaceous sediments of North America, the Arctic, the Antarctic and several localities in Europe. Trace element chemistry, XRD, SEM and stable isotope geochemistry were consistent in their results. Preservation of the origin...
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1991
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ftunivottawa:oai:ruor.uottawa.ca:10393/7784 2023-05-15T13:59:56+02:00 Cretaceous marine invertebrates: A geochemical perspective. Morrison, Joan Olivia. Veizer, J. 1991 279 p. application/pdf http://hdl.handle.net/10393/7784 https://doi.org/10.20381/ruor-15505 unknown University of Ottawa (Canada) Source: Dissertation Abstracts International, Volume: 53-03, Section: B, page: 1251. 9780315680470 http://hdl.handle.net/10393/7784 http://dx.doi.org/10.20381/ruor-15505 Paleontology Thesis 1991 ftunivottawa https://doi.org/10.20381/ruor-15505 2021-01-04T17:04:55Z A diagenetic evaluation was performed on marine fossil shell material from Cretaceous sediments of North America, the Arctic, the Antarctic and several localities in Europe. Trace element chemistry, XRD, SEM and stable isotope geochemistry were consistent in their results. Preservation of the original shell material of the low-Mg calcite organisms, brachiopods and belemnites, and the numerous aragonitic organisms was slightly variable with the majority of samples well preserved. Those samples that were altered underwent diagenetic stabilization in both reducing and oxic environments. Using the chemical data from only well preserved fossil shell material, basin paleo-reconstructions showed that from Aptian to Maastrichtian time, the Cretaceous seas were generally aerobic with some dysaerobia evident at the sediment/water interface and in the shallow sediment column. Paleosalinities fluctuated from brackish to normal marine, especially in the Western Interior Seaway of North America and the Paris Basin. The Lower Saxony basin, the Arctic and Antarctic were mainly normal marine with brackish conditions developing on occasion. Paleotemperatures determined from $\partial\sp $O data of preserved aragonite and low-Mg calcite shell material, also showed some variance. The Arctic and Antarctic were coolest, with Campanian/Maastrichtian temperatures about 12 or 13$\sp\circ$C, whereas the Lower Saxony basin and the Western Interior Seaway were slightly warmer, ranging from 11 to 20$\sp\circ$C. The Barremian/Aptian appeared to be the warmest time and a cooling trend was fairly consistent from then on. Thesis Antarc* Antarctic Arctic uO Research (University of Ottawa - uOttawa) Antarctic Arctic The Antarctic |
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uO Research (University of Ottawa - uOttawa) |
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Paleontology |
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Paleontology Morrison, Joan Olivia. Cretaceous marine invertebrates: A geochemical perspective. |
topic_facet |
Paleontology |
description |
A diagenetic evaluation was performed on marine fossil shell material from Cretaceous sediments of North America, the Arctic, the Antarctic and several localities in Europe. Trace element chemistry, XRD, SEM and stable isotope geochemistry were consistent in their results. Preservation of the original shell material of the low-Mg calcite organisms, brachiopods and belemnites, and the numerous aragonitic organisms was slightly variable with the majority of samples well preserved. Those samples that were altered underwent diagenetic stabilization in both reducing and oxic environments. Using the chemical data from only well preserved fossil shell material, basin paleo-reconstructions showed that from Aptian to Maastrichtian time, the Cretaceous seas were generally aerobic with some dysaerobia evident at the sediment/water interface and in the shallow sediment column. Paleosalinities fluctuated from brackish to normal marine, especially in the Western Interior Seaway of North America and the Paris Basin. The Lower Saxony basin, the Arctic and Antarctic were mainly normal marine with brackish conditions developing on occasion. Paleotemperatures determined from $\partial\sp $O data of preserved aragonite and low-Mg calcite shell material, also showed some variance. The Arctic and Antarctic were coolest, with Campanian/Maastrichtian temperatures about 12 or 13$\sp\circ$C, whereas the Lower Saxony basin and the Western Interior Seaway were slightly warmer, ranging from 11 to 20$\sp\circ$C. The Barremian/Aptian appeared to be the warmest time and a cooling trend was fairly consistent from then on. |
author2 |
Veizer, J. |
format |
Thesis |
author |
Morrison, Joan Olivia. |
author_facet |
Morrison, Joan Olivia. |
author_sort |
Morrison, Joan Olivia. |
title |
Cretaceous marine invertebrates: A geochemical perspective. |
title_short |
Cretaceous marine invertebrates: A geochemical perspective. |
title_full |
Cretaceous marine invertebrates: A geochemical perspective. |
title_fullStr |
Cretaceous marine invertebrates: A geochemical perspective. |
title_full_unstemmed |
Cretaceous marine invertebrates: A geochemical perspective. |
title_sort |
cretaceous marine invertebrates: a geochemical perspective. |
publisher |
University of Ottawa (Canada) |
publishDate |
1991 |
url |
http://hdl.handle.net/10393/7784 https://doi.org/10.20381/ruor-15505 |
geographic |
Antarctic Arctic The Antarctic |
geographic_facet |
Antarctic Arctic The Antarctic |
genre |
Antarc* Antarctic Arctic |
genre_facet |
Antarc* Antarctic Arctic |
op_relation |
Source: Dissertation Abstracts International, Volume: 53-03, Section: B, page: 1251. 9780315680470 http://hdl.handle.net/10393/7784 http://dx.doi.org/10.20381/ruor-15505 |
op_doi |
https://doi.org/10.20381/ruor-15505 |
_version_ |
1766268861756211200 |