Evidence map›Paper›PMID 37919271›Full record

ArticleNature communications2023

Atlantic-origin water extension into the Pacific Arctic induced an anomalous biogeochemical event.

Shigeto Nishino, Jinyoung Jung, Kyoung-Ho Cho, William J Williams, Amane Fujiwara, Akihiko Murata, Motoyo Itoh, Eiji Watanabe, Michio Aoyama, Michiyo Yamamoto-Kawai and 3 more

Abstract read
In one paragraph

Article in Nature communications, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.

0numbers the graph read from it
0cells of the map it votes in
5citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

5 citing papers in PubMed.

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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

13 authors.

Shigeto Nishino *Institute of Arctic Climate and Environment Research, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan. nishinos@jamstec.go.jp.ORCID http://orcid.org/0000-0002-0560-241X
Jinyoung Jung *Division of Ocean Sciences, Korea Polar Research Institute, Incheon, Republic of Korea.ORCID http://orcid.org/0000-0003-0284-1519
Kyoung-Ho ChoDivision of Ocean Sciences, Korea Polar Research Institute, Incheon, Republic of Korea.ORCID http://orcid.org/0000-0001-5527-5851
William J WilliamsInstitute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, BC, Canada.
Amane FujiwaraInstitute of Arctic Climate and Environment Research, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan.ORCID http://orcid.org/0000-0002-2307-6433
Akihiko MurataGlobal Ocean Observation Research Center, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan.ORCID http://orcid.org/0000-0002-5931-2784
Motoyo ItohInstitute of Arctic Climate and Environment Research, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan.
Eiji WatanabeInstitute of Arctic Climate and Environment Research, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan.ORCID http://orcid.org/0000-0002-7959-749X
Michio AoyamaGlobal Ocean Observation Research Center, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan.
Michiyo Yamamoto-KawaiDepartment of Ocean Sciences, Tokyo University of Marine Science and Technology, Tokyo, Japan.ORCID http://orcid.org/0000-0002-1035-2179
Takashi KikuchiInstitute of Arctic Climate and Environment Research, Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan.
Eun Jin YangDivision of Ocean Sciences, Korea Polar Research Institute, Incheon, Republic of Korea.ORCID http://orcid.org/0000-0002-8639-5968
Sung-Ho KangKorea Polar Research Institute, Incheon, Republic of Korea.

Funding

Ministry of Education, Culture, Sports, Science and Technology (MEXT) JPMXD1420318865Ministry of Oceans and Fisheries (MOF) KOPRI1525011760
6 · The paper itself

Abstract

The Arctic Ocean is facing dramatic environmental and ecosystem changes. In this context, an international multiship survey project was undertaken in 2020 to obtain current baseline data. During the survey, unusually low dissolved oxygen and acidified water were found in a high-seas fishable area of the western (Pacific-side) Arctic Ocean. Herein, we show that the Beaufort Gyre shrinks to the east of an ocean ridge and forms a front between the water within the gyre and the water from the eastern (Atlantic-side) Arctic. That phenomenon triggers a frontal northward flow along the ocean ridge. This flow likely transports the low oxygen and acidified water toward the high-seas fishable area; similar biogeochemical properties had previously been observed only on the shelf-slope north of the East Siberian Sea.

Identifiers

PMID37919271
PMCPMC10622542

What OpenQuestion holds

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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.