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a. Faunal abundance of selected taxa in relation to near-bottom temperature during summer sediment collection in the northern Bering and Chukchi Seas (n = 211, 26,170 total specimens, 1990–2018, ≥30 specimens/sample). b. Faunal abundance in relation to salinity. c. Faunal abundance in relation to se...
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ftsmithonian:oai:figshare.com:article/14591666 2023-05-15T15:54:30+02:00 S1 Fig - Laura Gemery (10798130) Thomas M. Cronin (3261858) Lee W. Cooper (8748120) Harry J. Dowsett (3274131) Jacqueline M. Grebmeier (8748126) 2021-05-13T17:49:20Z https://doi.org/10.1371/journal.pone.0251164.s001 unknown https://figshare.com/articles/journal_contribution/S1_Fig_-/14591666 doi:10.1371/journal.pone.0251164.s001 CC BY 4.0 CC-BY Evolutionary Biology Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified future sampling studies bottom water temperatures water mass characteristics Pacific species M Beaufort Seas Ostracoda synoptic ordination analyses water mass properties future ecosystem changes Chukchi Sea region future benthic monitoring efforts U.S 300 surface sediment samples summer water masses ostracode species Text Journal contribution 2021 ftsmithonian https://doi.org/10.1371/journal.pone.0251164.s001 2021-05-21T14:54:41Z a. Faunal abundance of selected taxa in relation to near-bottom temperature during summer sediment collection in the northern Bering and Chukchi Seas (n = 211, 26,170 total specimens, 1990–2018, ≥30 specimens/sample). b. Faunal abundance in relation to salinity. c. Faunal abundance in relation to sediment type. Ostracode species abundance plotted against the percent sediment modal grain size of phi 0–4, where 0 represents gravel and rocks, 1 = coarse sand, 2 = medium sand, 3–4 = finer sand. Phi ≥5 (not shown) represents the very fine silty mud and clay sediment fraction typical of offshore or interior areas of the continental shelf. (PDF) Other Non-Article Part of Journal/Newspaper Chukchi Chukchi Sea Unknown Chukchi Sea Pacific |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftsmithonian |
language |
unknown |
topic |
Evolutionary Biology Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified future sampling studies bottom water temperatures water mass characteristics Pacific species M Beaufort Seas Ostracoda synoptic ordination analyses water mass properties future ecosystem changes Chukchi Sea region future benthic monitoring efforts U.S 300 surface sediment samples summer water masses ostracode species |
spellingShingle |
Evolutionary Biology Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified future sampling studies bottom water temperatures water mass characteristics Pacific species M Beaufort Seas Ostracoda synoptic ordination analyses water mass properties future ecosystem changes Chukchi Sea region future benthic monitoring efforts U.S 300 surface sediment samples summer water masses ostracode species Laura Gemery (10798130) Thomas M. Cronin (3261858) Lee W. Cooper (8748120) Harry J. Dowsett (3274131) Jacqueline M. Grebmeier (8748126) S1 Fig - |
topic_facet |
Evolutionary Biology Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified future sampling studies bottom water temperatures water mass characteristics Pacific species M Beaufort Seas Ostracoda synoptic ordination analyses water mass properties future ecosystem changes Chukchi Sea region future benthic monitoring efforts U.S 300 surface sediment samples summer water masses ostracode species |
description |
a. Faunal abundance of selected taxa in relation to near-bottom temperature during summer sediment collection in the northern Bering and Chukchi Seas (n = 211, 26,170 total specimens, 1990–2018, ≥30 specimens/sample). b. Faunal abundance in relation to salinity. c. Faunal abundance in relation to sediment type. Ostracode species abundance plotted against the percent sediment modal grain size of phi 0–4, where 0 represents gravel and rocks, 1 = coarse sand, 2 = medium sand, 3–4 = finer sand. Phi ≥5 (not shown) represents the very fine silty mud and clay sediment fraction typical of offshore or interior areas of the continental shelf. (PDF) |
format |
Other Non-Article Part of Journal/Newspaper |
author |
Laura Gemery (10798130) Thomas M. Cronin (3261858) Lee W. Cooper (8748120) Harry J. Dowsett (3274131) Jacqueline M. Grebmeier (8748126) |
author_facet |
Laura Gemery (10798130) Thomas M. Cronin (3261858) Lee W. Cooper (8748120) Harry J. Dowsett (3274131) Jacqueline M. Grebmeier (8748126) |
author_sort |
Laura Gemery (10798130) |
title |
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title_full |
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title_full_unstemmed |
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title_sort |
s1 fig - |
publishDate |
2021 |
url |
https://doi.org/10.1371/journal.pone.0251164.s001 |
geographic |
Chukchi Sea Pacific |
geographic_facet |
Chukchi Sea Pacific |
genre |
Chukchi Chukchi Sea |
genre_facet |
Chukchi Chukchi Sea |
op_relation |
https://figshare.com/articles/journal_contribution/S1_Fig_-/14591666 doi:10.1371/journal.pone.0251164.s001 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1371/journal.pone.0251164.s001 |
_version_ |
1766389699214049280 |