increased, but also became more pulsed or seasonal, peaking at 9–8 Ma, while deep and intermediate waters may have become more ventilated. The first phase of faunal change (14–13 Ma) was coeval with the global increase in benthic foraminiferal oxygen isotope The Miocene was a time of major changes i...
Main Authors: | , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
2006
|
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.1215 http://ethomas.web.wesleyan.edu/Smartetal07.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.525.1215 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.525.1215 2023-05-15T13:42:35+02:00 Ellen Thomas B Anthony T. S. Ramsay C The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.1215 http://ethomas.web.wesleyan.edu/Smartetal07.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.1215 http://ethomas.web.wesleyan.edu/Smartetal07.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://ethomas.web.wesleyan.edu/Smartetal07.pdf text 2006 ftciteseerx 2016-01-08T10:19:16Z increased, but also became more pulsed or seasonal, peaking at 9–8 Ma, while deep and intermediate waters may have become more ventilated. The first phase of faunal change (14–13 Ma) was coeval with the global increase in benthic foraminiferal oxygen isotope The Miocene was a time of major changes in the established (e.g., Ramstein et al., 1997). The East Antarctic Ice Sheet (EAIS), and hence steep thermal gradients between high and low latitudes, probably Palaeogeography, Palaeoclimatology, Palaeoeocean–atmosphere system. By early Miocene timesvalues, worldwide turnover in benthic foraminiferal faunas, and possibly increased production of Antarctic Bottom Water (AABW) and Northern Component Water (NCW). The overall faunal turnover may reflect the composite faunal response to increased food input resulting from heightened productivity and increased bottom water ventilation associated with a combination of monsoonal intensification, global cooling and changes in ocean circulation, but there is no unequivocal evidence for the presence of Tethyan Text Antarc* Antarctic Ice Sheet Unknown Antarctic East Antarctic Ice Sheet |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
increased, but also became more pulsed or seasonal, peaking at 9–8 Ma, while deep and intermediate waters may have become more ventilated. The first phase of faunal change (14–13 Ma) was coeval with the global increase in benthic foraminiferal oxygen isotope The Miocene was a time of major changes in the established (e.g., Ramstein et al., 1997). The East Antarctic Ice Sheet (EAIS), and hence steep thermal gradients between high and low latitudes, probably Palaeogeography, Palaeoclimatology, Palaeoeocean–atmosphere system. By early Miocene timesvalues, worldwide turnover in benthic foraminiferal faunas, and possibly increased production of Antarctic Bottom Water (AABW) and Northern Component Water (NCW). The overall faunal turnover may reflect the composite faunal response to increased food input resulting from heightened productivity and increased bottom water ventilation associated with a combination of monsoonal intensification, global cooling and changes in ocean circulation, but there is no unequivocal evidence for the presence of Tethyan |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Ellen Thomas B Anthony T. S. Ramsay C |
spellingShingle |
Ellen Thomas B Anthony T. S. Ramsay C |
author_facet |
Ellen Thomas B Anthony T. S. Ramsay C |
author_sort |
Ellen Thomas B |
publishDate |
2006 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.1215 http://ethomas.web.wesleyan.edu/Smartetal07.pdf |
geographic |
Antarctic East Antarctic Ice Sheet |
geographic_facet |
Antarctic East Antarctic Ice Sheet |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
http://ethomas.web.wesleyan.edu/Smartetal07.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.1215 http://ethomas.web.wesleyan.edu/Smartetal07.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766169876568735744 |