Evidence map›Paper›PMID 29308272›Full record

ArticleRoyal Society open science2017

Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll.

Junichi Miyazaki, Shinsuke Kawagucci, Akiko Makabe, Ayu Takahashi, Kazuya Kitada, Junji Torimoto, Yohei Matsui, Eiji Tasumi, Takazo Shibuya, Kentaro Nakamura and 11 more

Abstract read
In one paragraph

Article in Royal Society open science, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 13 papers.

0numbers the graph read from it
0cells of the map it votes in
13citing 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

13 citing papers in PubMed.

  1. Article
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  7. New records ofZooKeys · 2024
    Article
  8. Article
  9. Article
  10. Heterotrophic Sulfur Oxidation ofFrontiers in microbiology · 2022
    Article
  11. Article
  12. Article
  13. Article
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

21 authors.

Junichi MiyazakiDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Shinsuke KawagucciDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Akiko MakabeProject Team for Development of New-generation Research Protocol for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Ayu TakahashiResearch and Development Center for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Kazuya KitadaResearch and Development Center for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Junji TorimotoProject Team for Development of New-generation Research Protocol for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Yohei MatsuiResearch and Development Center for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Eiji TasumiDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Takazo ShibuyaDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Kentaro NakamuraResearch and Development Center for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Shunsuke HoraiDepartment of Earth and Planetary Sciences, School of Science, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan.
Shun SatoDepartment of Earth and Planetary Sciences, School of Science, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan.
Jun-Ichiro IshibashiDepartment of Earth and Planetary Sciences, School of Science, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan.
Hayato KanzakiLaboratory of Marine Environmental Microbiology, Division of Applied Biosciences, Graduate School of Agriculture, Kyoto University, Oiwake-cho, Kitashirakawa, Sakyo-ku, Kyoto 606-8502, Japan.
Satoshi NakagawaDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Miho HiraiResearch and Development Center for Marine Biosciences, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Yoshihiro TakakiDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Kyoko OkinoAtmosphere and Ocean Research Institute, The University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa 277-8564, Japan.
Hiromi Kayama WatanabeResearch and Development Center for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Hidenori KumagaiResearch and Development Center for Submarine Resources, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.
Chong ChenDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR), 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.ORCID 0000-0002-5035-4021

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Since the initial discovery of hydrothermal vents in 1977, these 'extreme' chemosynthetic systems have been a focus of interdisciplinary research. The Okinawa Trough (OT), located in the semi-enclosed East China Sea between the Eurasian continent and the Ryukyu arc, hosts more than 20 known vent sites but all within a relatively narrow depth range (600-1880 m). Depth is a significant factor in determining fluid temperature and chemistry, as well as biological composition. However, due to the narrow depth range of known sites, the actual influence of depth here has been poorly resolved. Here, the Yokosuka site (2190 m), the first OT vent exceeding 2000 m depth is reported. A highly active hydrothermal vent site centred around four active vent chimneys reaching 364°C in temperature, it is the hottest in the OT. Notable Cl depletion (130 mM) and both high H

Indexed as

biodiversitychemosynthetic ecosystemfluid chemistryhydrothermal ventmicrobial compositionsulfide deposit

Identifiers

PMID29308272
PMCPMC5750039

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Registered trials

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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.