Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015
The Pacific sector of the Arctic Ocean is experiencing major reductions in seasonal sea ice extent and increases in sea surface temperatures. One of the key uncertainties in this region is how the marine ecosystem will respond to seasonal shifts in the timing of spring sea ice retreat and/or delays...
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2019
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dataone:doi:10.18739/A2HH6C58X 2024-11-03T19:45:06+00:00 Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 Jacqueline M. Grebmeier Lee W. Cooper DBO 1 - South of St. Lawrence Island, Bering Sea DBO 2 - Chirikov Basin, Northern Bering Sea DBO 3 - Southern Chukchi Sea DBO 4 - Northeast Chukchi Sea DBO 5 - Barrow Canyon, Chukchi Sea ENVELOPE(-176.147,-172.187,63.769,61.847) BEGINDATE: 2015-07-14T00:00:00Z ENDDATE: 2015-07-21T00:00:00Z 2019-01-01T00:00:00Z https://doi.org/10.18739/A2HH6C58X unknown Arctic Data Center sediment grain size total organic carbon total organic nitrogen C/N surface sediment chlorophyll Dataset 2019 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2HH6C58X 2024-11-03T19:12:40Z The Pacific sector of the Arctic Ocean is experiencing major reductions in seasonal sea ice extent and increases in sea surface temperatures. One of the key uncertainties in this region is how the marine ecosystem will respond to seasonal shifts in the timing of spring sea ice retreat and/or delays in fall sea ice formation. Variations in upper ocean water hydrography, planktonic production, pelagic-benthic coupling and sediment carbon cycling are all influenced by sea ice and temperature change. To more systematically track the broad biological response to sea ice retreat and associated environmental change, an international consortium of scientists have developed a coordinated Distributed Biological Observatory(DBO) that includes selected biological measurements at multiple trophic levels, along with satellite and mooring measurements. The DBO currently focuses on five regional biological "hotspot" locations along a latitudinal gradient that allows for consistent sampling and monitoring at five biologically productive locations across a latitudinal gradient: DBO 1 (SLIP)-south of St. Lawrence Island (SLI), DBO2 (Chirikov)-north of SLI, DBO3 (southern Chukchi Sea), DBO4-NE Chukchi Sea,and DBO5-Barrow Canyon. This dataset contains summary measurements of surface sediment collected at each station for the identified cruise, including: sediment grain size (≤0 phi, 1 phi, 2 phi, 3 phi, 4 phi, ≣5 phi, 1-4 phi, and modal phi size), total organic carbon (TOC), total organic nitrogen (TON), C/N and surface sediment chlorophyll (chl a). Surface sediment chlorophyll (chl a) content is scaled up to mg Chl a/m2. Dataset Arctic Arctic Ocean Bering Sea Chukchi Chukchi Sea Sea ice St Lawrence Island Arctic Data Center (via DataONE) Arctic Arctic Ocean Bering Sea Chukchi Sea Pacific Lawrence Island ENVELOPE(-103.718,-103.718,56.967,56.967) Barrow Canyon ENVELOPE(-154.000,-154.000,72.500,72.500) ENVELOPE(-176.147,-172.187,63.769,61.847) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
sediment grain size total organic carbon total organic nitrogen C/N surface sediment chlorophyll |
spellingShingle |
sediment grain size total organic carbon total organic nitrogen C/N surface sediment chlorophyll Jacqueline M. Grebmeier Lee W. Cooper Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 |
topic_facet |
sediment grain size total organic carbon total organic nitrogen C/N surface sediment chlorophyll |
description |
The Pacific sector of the Arctic Ocean is experiencing major reductions in seasonal sea ice extent and increases in sea surface temperatures. One of the key uncertainties in this region is how the marine ecosystem will respond to seasonal shifts in the timing of spring sea ice retreat and/or delays in fall sea ice formation. Variations in upper ocean water hydrography, planktonic production, pelagic-benthic coupling and sediment carbon cycling are all influenced by sea ice and temperature change. To more systematically track the broad biological response to sea ice retreat and associated environmental change, an international consortium of scientists have developed a coordinated Distributed Biological Observatory(DBO) that includes selected biological measurements at multiple trophic levels, along with satellite and mooring measurements. The DBO currently focuses on five regional biological "hotspot" locations along a latitudinal gradient that allows for consistent sampling and monitoring at five biologically productive locations across a latitudinal gradient: DBO 1 (SLIP)-south of St. Lawrence Island (SLI), DBO2 (Chirikov)-north of SLI, DBO3 (southern Chukchi Sea), DBO4-NE Chukchi Sea,and DBO5-Barrow Canyon. This dataset contains summary measurements of surface sediment collected at each station for the identified cruise, including: sediment grain size (≤0 phi, 1 phi, 2 phi, 3 phi, 4 phi, ≣5 phi, 1-4 phi, and modal phi size), total organic carbon (TOC), total organic nitrogen (TON), C/N and surface sediment chlorophyll (chl a). Surface sediment chlorophyll (chl a) content is scaled up to mg Chl a/m2. |
format |
Dataset |
author |
Jacqueline M. Grebmeier Lee W. Cooper |
author_facet |
Jacqueline M. Grebmeier Lee W. Cooper |
author_sort |
Jacqueline M. Grebmeier |
title |
Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 |
title_short |
Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 |
title_full |
Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 |
title_fullStr |
Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 |
title_full_unstemmed |
Surface sediment samples collected from the CCGS Sir Wilfrid Laurier, Northern Bering Sea to Chukchi Sea, 2015 |
title_sort |
surface sediment samples collected from the ccgs sir wilfrid laurier, northern bering sea to chukchi sea, 2015 |
publisher |
Arctic Data Center |
publishDate |
2019 |
url |
https://doi.org/10.18739/A2HH6C58X |
op_coverage |
DBO 1 - South of St. Lawrence Island, Bering Sea DBO 2 - Chirikov Basin, Northern Bering Sea DBO 3 - Southern Chukchi Sea DBO 4 - Northeast Chukchi Sea DBO 5 - Barrow Canyon, Chukchi Sea ENVELOPE(-176.147,-172.187,63.769,61.847) BEGINDATE: 2015-07-14T00:00:00Z ENDDATE: 2015-07-21T00:00:00Z |
long_lat |
ENVELOPE(-103.718,-103.718,56.967,56.967) ENVELOPE(-154.000,-154.000,72.500,72.500) ENVELOPE(-176.147,-172.187,63.769,61.847) |
geographic |
Arctic Arctic Ocean Bering Sea Chukchi Sea Pacific Lawrence Island Barrow Canyon |
geographic_facet |
Arctic Arctic Ocean Bering Sea Chukchi Sea Pacific Lawrence Island Barrow Canyon |
genre |
Arctic Arctic Ocean Bering Sea Chukchi Chukchi Sea Sea ice St Lawrence Island |
genre_facet |
Arctic Arctic Ocean Bering Sea Chukchi Chukchi Sea Sea ice St Lawrence Island |
op_doi |
https://doi.org/10.18739/A2HH6C58X |
_version_ |
1814734586558545920 |