A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age
The Wordiekammen Formation, a carbonate ramp on Spitsbergen developed on the Northern Pangaean margin in Moscovian (Carboniferous) through Sakmarian (Permian) time at a paleolatitude of 30-358 N. The study site on the Nordfjorden High was isolated from any source of fluvio-deltaic input, such that d...
Published in: | Journal of Sedimentary Research |
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2020
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Online Access: | https://curis.ku.dk/portal/da/publications/a-record-of-dust-deposition-in-northern-midlatitude-pangaea-during-peak-icehouse-conditions-of-the-late-paleozoic-ice-age(d51bb7a4-2006-4362-b9d2-ecde5432aac0).html https://doi.org/10.2110/jsr.2020.15 |
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ftcopenhagenunip:oai:pure.atira.dk:publications/d51bb7a4-2006-4362-b9d2-ecde5432aac0 2024-06-09T07:46:28+00:00 A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age Oordt, Andrew J. Soreghan, Gerilyn S. Stemmerik, Lars Hinnov, Linda A. 2020 https://curis.ku.dk/portal/da/publications/a-record-of-dust-deposition-in-northern-midlatitude-pangaea-during-peak-icehouse-conditions-of-the-late-paleozoic-ice-age(d51bb7a4-2006-4362-b9d2-ecde5432aac0).html https://doi.org/10.2110/jsr.2020.15 eng eng info:eu-repo/semantics/closedAccess Oordt , A J , Soreghan , G S , Stemmerik , L & Hinnov , L A 2020 , ' A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age ' , Journal of Sedimentary Research , vol. 90 , no. 4 , pp. 337-363 . https://doi.org/10.2110/jsr.2020.15 article 2020 ftcopenhagenunip https://doi.org/10.2110/jsr.2020.15 2024-05-16T11:29:20Z The Wordiekammen Formation, a carbonate ramp on Spitsbergen developed on the Northern Pangaean margin in Moscovian (Carboniferous) through Sakmarian (Permian) time at a paleolatitude of 30-358 N. The study site on the Nordfjorden High was isolated from any source of fluvio-deltaic input, such that detrital material that occurs in this system experienced eolian transport, thus forming a proxy for atmospheric dust loading. We analyzed two intervals, of Moscovian (10 m) and Asselian (27 m) age, at 20 cm resolution, and identified five mid-ramp subtidal facies organized in upwardly shallowing, high-frequency sequences 3-5 m thick. High-frequency sequence boundaries commonly exhibit signs of subaerial exposure (e.g., Microcodium) developed atop subtidal facies, recording glacioeustatic falls (glacial phases), although the Moscovian section has a severe karst overprint attributable to prolonged exposure on a paleohigh. Samples were processed to isolate the silicate-mineral fraction (SMF), which includes both detrital silicate material and authigenic silica mostly in the form of (fine-sand-size) doubly terminated quartz crystals. Detrital cores in these crystals, together with other evidence, indicate recrystallization from fine-grained (silt- and clay-size) dust. Analysis of the dust record demonstrates that the Asselian (peak icehouse) had a significantly higher atmospheric dust load than the Moscovian (moderate icehouse). In the Asselian interval, dust input varies commensurate with glacial-interglacial cyclicity. Highest dust contents correspond to transgressive facies immediately above sequence boundaries, indicating peak atmospheric dust loading at lowstand to incipient interglacial times. Provenance data from detrital-zircon and whole-rock geochemistry indicate two distinct source regions for the dust. Dust from the Moscovian and lower Asselian intervals reflects a continental island-arc signature consistent with sourcing from the basement of northeast Greenland. Dust from the upper Asselian interval is more ... Article in Journal/Newspaper Greenland Spitsbergen University of Copenhagen: Research Greenland Wordiekammen ENVELOPE(16.756,16.756,78.697,78.697) Journal of Sedimentary Research 90 4 337 363 |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
description |
The Wordiekammen Formation, a carbonate ramp on Spitsbergen developed on the Northern Pangaean margin in Moscovian (Carboniferous) through Sakmarian (Permian) time at a paleolatitude of 30-358 N. The study site on the Nordfjorden High was isolated from any source of fluvio-deltaic input, such that detrital material that occurs in this system experienced eolian transport, thus forming a proxy for atmospheric dust loading. We analyzed two intervals, of Moscovian (10 m) and Asselian (27 m) age, at 20 cm resolution, and identified five mid-ramp subtidal facies organized in upwardly shallowing, high-frequency sequences 3-5 m thick. High-frequency sequence boundaries commonly exhibit signs of subaerial exposure (e.g., Microcodium) developed atop subtidal facies, recording glacioeustatic falls (glacial phases), although the Moscovian section has a severe karst overprint attributable to prolonged exposure on a paleohigh. Samples were processed to isolate the silicate-mineral fraction (SMF), which includes both detrital silicate material and authigenic silica mostly in the form of (fine-sand-size) doubly terminated quartz crystals. Detrital cores in these crystals, together with other evidence, indicate recrystallization from fine-grained (silt- and clay-size) dust. Analysis of the dust record demonstrates that the Asselian (peak icehouse) had a significantly higher atmospheric dust load than the Moscovian (moderate icehouse). In the Asselian interval, dust input varies commensurate with glacial-interglacial cyclicity. Highest dust contents correspond to transgressive facies immediately above sequence boundaries, indicating peak atmospheric dust loading at lowstand to incipient interglacial times. Provenance data from detrital-zircon and whole-rock geochemistry indicate two distinct source regions for the dust. Dust from the Moscovian and lower Asselian intervals reflects a continental island-arc signature consistent with sourcing from the basement of northeast Greenland. Dust from the upper Asselian interval is more ... |
format |
Article in Journal/Newspaper |
author |
Oordt, Andrew J. Soreghan, Gerilyn S. Stemmerik, Lars Hinnov, Linda A. |
spellingShingle |
Oordt, Andrew J. Soreghan, Gerilyn S. Stemmerik, Lars Hinnov, Linda A. A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age |
author_facet |
Oordt, Andrew J. Soreghan, Gerilyn S. Stemmerik, Lars Hinnov, Linda A. |
author_sort |
Oordt, Andrew J. |
title |
A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age |
title_short |
A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age |
title_full |
A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age |
title_fullStr |
A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age |
title_full_unstemmed |
A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age |
title_sort |
record of dust deposition in northern, mid-latitude pangaea during peak icehouse conditions of the late paleozoic ice age |
publishDate |
2020 |
url |
https://curis.ku.dk/portal/da/publications/a-record-of-dust-deposition-in-northern-midlatitude-pangaea-during-peak-icehouse-conditions-of-the-late-paleozoic-ice-age(d51bb7a4-2006-4362-b9d2-ecde5432aac0).html https://doi.org/10.2110/jsr.2020.15 |
long_lat |
ENVELOPE(16.756,16.756,78.697,78.697) |
geographic |
Greenland Wordiekammen |
geographic_facet |
Greenland Wordiekammen |
genre |
Greenland Spitsbergen |
genre_facet |
Greenland Spitsbergen |
op_source |
Oordt , A J , Soreghan , G S , Stemmerik , L & Hinnov , L A 2020 , ' A record of dust deposition in northern, mid-latitude Pangaea during peak icehouse conditions of the late Paleozoic ice age ' , Journal of Sedimentary Research , vol. 90 , no. 4 , pp. 337-363 . https://doi.org/10.2110/jsr.2020.15 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.2110/jsr.2020.15 |
container_title |
Journal of Sedimentary Research |
container_volume |
90 |
container_issue |
4 |
container_start_page |
337 |
op_container_end_page |
363 |
_version_ |
1801376315918516224 |