OldBlackDog
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Not due to man made global warming.
Tropical Island Fossil Clues To Polar Ice And Sea Level
10.01.2015 10:38 Age: 21 days
Seychelles fossils reveal the past and possible future of polar ice and sea level with evidence of a rapid retreat of the Antarctic ice sheet in the past driving up sea levels, according to research
Click to enlarge. Andrea Dutton: evidence for rapid retreat of ice sheet. Courtesy: Andrea Dutton
From the University of Florida
The balmy islands of Seychelles couldn’t feel farther from Antarctica, but their fossil corals could reveal much about the fate of polar ice sheets.
About 125,000 years ago, the average global temperature was only slightly warmer, but sea levels rose high enough to submerge the locations of many of today’s coastal cities. Understanding what caused seas to rise then could shed light on how to protect those cities today.
By examining fossil corals found on the Indian Ocean islands, University of Florida geochemist Andrea Dutton found evidence that global mean sea level during that period peaked at 20 to 30 feet above current levels. Dutton’s team of international researchers concluded that rapid retreat of an unstable part of the Antarctic ice sheet was a major contributor to that sea-level rise.
“This occurred during a time when the average global temperature was only slightly warmer than at present,” Dutton said.
Dutton evaluated fossil corals in Seychelles because sea level in that region closely matches that of global mean sea level. Local patterns of sea-level change can differ from global trends because of variations in the Earth’s surface and gravity fields that occur when ice sheets grow and shrink.
In an article published in the January 2015 issue of Quaternary Science Reviews, the researchers concluded that while sea-level rise in the Last Interglacial period was driven by the same processes active today – thermal expansion of seawater, melting mountain glaciers and melting polar ice sheets in Greenland and Antarctica – most was driven by polar ice sheet melt. Their study, partially funded by the National Science Foundation, also suggests the Antarctic ice sheet partially collapsed early in that period.
“Following a rapid transition to high sea levels when the last interglacial period began, sea level continued rising steadily,” Dutton said. “The collapse of Antarctic ice occurred when the polar regions were a few degrees warmer than they are now — temperatures that we are likely to reach within a matter of decades.”
Several recent studies by other researchers suggest that process may have already started.
“We could be poised for another partial collapse of the Antarctic ice sheet,” Dutton said.
Highlights
Quarternary science reviews identifyies the following highlights from this research
Peak eustatic sea level (ESL) for MIS 5e estimated at ∼7.6 ± 1.7 m above present.
Polar ice sheets contributed ∼5–8 m of ice-equivalent sea level to this peak.
Partial collapse of Antarctic ice sheet may have occurred early in MIS 5e.
Gradual sea-level rise of ∼0.2 m ka−1 recorded between ∼129 and 125 ka.
Abstract
In the search for a record of eustatic sea level change on glacial–interglacial timescales, the Seychelles ranks as one of the best places on the planet to study. Owing to its location with respect to the former margins of Northern Hemisphere ice sheets that wax and wane on orbital cycles, the local—or relative—sea level history is predicted to lie within a few meters of the globally averaged eustatic signal during the Last Interglacial period. We have surveyed and dated Last Interglacial fossil corals to ascertain peak sea level and hence infer maximum retreat of polar ice sheets during this time interval. We observe a pattern of gradually rising sea level in the Seychelles between ∼129 and 125 thousand years ago (ka), with peak eustatic sea level attained after 125 ka at 7.6 ± 1.7 m higher than present. After accounting for thermal expansion and loss of mountain glaciers, this sea-level budget would require ∼5–8 m of polar ice sheet contribution, relative to today's volume, of which only ∼2 m came from the Greenland ice sheet. This result clearly identifies the Antarctic ice sheet as a significant source of melt water, most likely derived from one of the unstable, marine-based sectors in the West and/or East Antarctic ice sheet. Furthermore, the establishment of a +5.9 ± 1.7 m eustatic sea level position by 128.6 ± 0.8 ka would require that partial AIS collapse was coincident with the onset of the sea level highstand.
Citation
Tropical tales of polar ice: evidence of Last Interglacial polar ice sheet retreat recorded by fossil reefs of the granitic Seychelles islands by Andrea Duttona, Jody M. Webster, Dan Zwartz, Kurt Lambeck and Barbara Wohlfarth published in Quaternary Science Reviews Volume 107, 1 January 2015, Pages 182–196, doi:10.1016/j.quascirev.2014.10.025
Read the abstract and get the paper here.
Source
University of Florida news release here.
Tropical Island Fossil Clues To Polar Ice And Sea Level
10.01.2015 10:38 Age: 21 days
Seychelles fossils reveal the past and possible future of polar ice and sea level with evidence of a rapid retreat of the Antarctic ice sheet in the past driving up sea levels, according to research
Click to enlarge. Andrea Dutton: evidence for rapid retreat of ice sheet. Courtesy: Andrea Dutton
From the University of Florida
The balmy islands of Seychelles couldn’t feel farther from Antarctica, but their fossil corals could reveal much about the fate of polar ice sheets.
About 125,000 years ago, the average global temperature was only slightly warmer, but sea levels rose high enough to submerge the locations of many of today’s coastal cities. Understanding what caused seas to rise then could shed light on how to protect those cities today.
By examining fossil corals found on the Indian Ocean islands, University of Florida geochemist Andrea Dutton found evidence that global mean sea level during that period peaked at 20 to 30 feet above current levels. Dutton’s team of international researchers concluded that rapid retreat of an unstable part of the Antarctic ice sheet was a major contributor to that sea-level rise.
“This occurred during a time when the average global temperature was only slightly warmer than at present,” Dutton said.
Dutton evaluated fossil corals in Seychelles because sea level in that region closely matches that of global mean sea level. Local patterns of sea-level change can differ from global trends because of variations in the Earth’s surface and gravity fields that occur when ice sheets grow and shrink.
In an article published in the January 2015 issue of Quaternary Science Reviews, the researchers concluded that while sea-level rise in the Last Interglacial period was driven by the same processes active today – thermal expansion of seawater, melting mountain glaciers and melting polar ice sheets in Greenland and Antarctica – most was driven by polar ice sheet melt. Their study, partially funded by the National Science Foundation, also suggests the Antarctic ice sheet partially collapsed early in that period.
“Following a rapid transition to high sea levels when the last interglacial period began, sea level continued rising steadily,” Dutton said. “The collapse of Antarctic ice occurred when the polar regions were a few degrees warmer than they are now — temperatures that we are likely to reach within a matter of decades.”
Several recent studies by other researchers suggest that process may have already started.
“We could be poised for another partial collapse of the Antarctic ice sheet,” Dutton said.
Highlights
Quarternary science reviews identifyies the following highlights from this research
Peak eustatic sea level (ESL) for MIS 5e estimated at ∼7.6 ± 1.7 m above present.
Polar ice sheets contributed ∼5–8 m of ice-equivalent sea level to this peak.
Partial collapse of Antarctic ice sheet may have occurred early in MIS 5e.
Gradual sea-level rise of ∼0.2 m ka−1 recorded between ∼129 and 125 ka.
Abstract
In the search for a record of eustatic sea level change on glacial–interglacial timescales, the Seychelles ranks as one of the best places on the planet to study. Owing to its location with respect to the former margins of Northern Hemisphere ice sheets that wax and wane on orbital cycles, the local—or relative—sea level history is predicted to lie within a few meters of the globally averaged eustatic signal during the Last Interglacial period. We have surveyed and dated Last Interglacial fossil corals to ascertain peak sea level and hence infer maximum retreat of polar ice sheets during this time interval. We observe a pattern of gradually rising sea level in the Seychelles between ∼129 and 125 thousand years ago (ka), with peak eustatic sea level attained after 125 ka at 7.6 ± 1.7 m higher than present. After accounting for thermal expansion and loss of mountain glaciers, this sea-level budget would require ∼5–8 m of polar ice sheet contribution, relative to today's volume, of which only ∼2 m came from the Greenland ice sheet. This result clearly identifies the Antarctic ice sheet as a significant source of melt water, most likely derived from one of the unstable, marine-based sectors in the West and/or East Antarctic ice sheet. Furthermore, the establishment of a +5.9 ± 1.7 m eustatic sea level position by 128.6 ± 0.8 ka would require that partial AIS collapse was coincident with the onset of the sea level highstand.
Citation
Tropical tales of polar ice: evidence of Last Interglacial polar ice sheet retreat recorded by fossil reefs of the granitic Seychelles islands by Andrea Duttona, Jody M. Webster, Dan Zwartz, Kurt Lambeck and Barbara Wohlfarth published in Quaternary Science Reviews Volume 107, 1 January 2015, Pages 182–196, doi:10.1016/j.quascirev.2014.10.025
Read the abstract and get the paper here.
Source
University of Florida news release here.