Evidence map›Paper›PMID 29760114›Full record

ArticlePhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2018

A 'shallow bathtub ring' of local sedimentary iron input maintains the Palmer Deep biological hotspot on the West Antarctic Peninsula shelf.

Robert M Sherrell, Amber L Annett, Jessica N Fitzsimmons, Vincent J Roccanova, Michael P Meredith

Abstract read
In one paragraph

Article in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2018. 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. Warming substantially amplifies Antarctic coastal polynyas as key carbon sinks.Proceedings of the National Academy of Sciences of the United States of America · 2025
    Article
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  10. Shelf-ocean exchange and hydrography west of the Antarctic Peninsula: a review.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2018
    Review
  11. The marine system of the West Antarctic Peninsula: status and strategy for progress.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2018
    Article
  12. Article
  13. Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2018
    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

5 authors.

Robert M SherrellDepartment of Marine and Coastal Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA sherrell@marine.rutgers.edu.ORCID http://orcid.org/0000-0002-2498-744X
Amber L AnnettDepartment of Marine and Coastal Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA.
Jessica N FitzsimmonsDepartment of Marine and Coastal Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA.
Vincent J RoccanovaDepartment of Marine and Coastal Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA.
Michael P MeredithBritish Antarctic Survey, Cambridge, UK.ORCID http://orcid.org/0000-0002-7342-7756

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Palmer Deep (PD) is one of several regional hotspots of biological productivity along the inner shelf of the West Antarctic Peninsula. The proximity of hotspots to shelf-crossing deep troughs has led to the 'canyon hypothesis', which proposes that circumpolar deep water flowing shoreward along the canyons is upwelled on the inner shelf, carrying nutrients including iron (Fe) to surface waters, maintaining phytoplankton blooms. We present here full-depth profiles of dissolved and particulate Fe and manganese (Mn) from eight stations around PD, sampled in January and early February of 2015 and 2016, allowing the first detailed evaluation of Fe sources to the area's euphotic zone. We show that upwelling of deep water does not control Fe flux to the surface; instead, shallow sediment-sourced Fe inputs are transported horizontally from surrounding coastlines, creating strong vertical gradients of dissolved Fe within the upper 100 m that supply this limiting nutrient to the local ecosystem. The supply of bioavailable Fe is, therefore, not significantly related to the canyon transport of deep water. Near shore time-series samples reveal that local glacial meltwater appears to be an important Mn source but, surprisingly, is not a large direct Fe input to this biological hotspot.This article is part of the theme issue 'The marine system of the West Antarctic Peninsula: status and strategy for progress in a region of rapid change'.

Indexed as

Antarcticbiogeochemistryironmanganesephytoplanktonsediment

Identifiers

PMID29760114
PMCPMC5954470

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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.