Evidence map›Paper›PMID 39095508›Full record

ArticleScientific reports2024

The latest shallow-sea isocrinids from the Miocene of Paratethys and implications to the Mesozoic marine revolution.

Mariusz A Salamon, Urszula Radwańska, Karolina Paszcza, Marcin Krajewski, Tomasz Brachaniec, Robert Niedźwiedzki, Przemysław Gorzelak

Abstract read
In one paragraph

Article in Scientific reports, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing 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

3 citing papers in PubMed.

  1. Article
  2. Article
  3. 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

7 authors.

Mariusz A SalamonFaculty of Earth Sciences, Laboratory of Palaeontology and Stratigraphy, University of Silesia in Katowice, Będzińska 60, 41-200, Sosnowiec, Poland.
Urszula RadwańskaFaculty of Geology, Department of Historical, Regional Geology and Paleontology, University of Warsaw, Żwirki i Wigury93, 02-089, Warszawa, Poland.
Karolina PaszczaFaculty of Earth Sciences, Laboratory of Palaeontology and Stratigraphy, University of Silesia in Katowice, Będzińska 60, 41-200, Sosnowiec, Poland.
Marcin KrajewskiFaculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059, Kraków, Poland.
Tomasz BrachaniecFaculty of Earth Sciences, Laboratory of Palaeontology and Stratigraphy, University of Silesia in Katowice, Będzińska 60, 41-200, Sosnowiec, Poland.
Robert NiedźwiedzkiFaculty of Earth Sciences and Environmental Management, Institute of Geological Sciences, Wrocław University, Cybulskiego 30, 50-205, Wrocław, Poland.
Przemysław GorzelakInstitute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, 00-818, Warsaw, Poland. pgorzelak@twarda.pan.pl.

Funding

AGH-UST 16.16.140.315Narodowe Centrum Nauki 2020/39/B/ST10/00006
6 · The paper itself

Abstract

The predation-driven Mesozoic marine revolution (MMR) is believed to have induced a dramatic change in the bathymetric distribution of many shallow marine invertebrates since the late Mesozoic. For instance, stalked crinoids - isocrinids (Isocrinida) have undergone a striking decline in shallow-sea environments and today they are restricted to deep-sea settings (below 100 m depth). However, the timing and synchronicity of this shift are a matter of debate. A delayed onset of MMR and/or shifts to a retrograde, low-predation community structure during the Paleogene in the Southern Ocean were invoked. In particular, recent data from the Southern Hemisphere suggest that the environmental restriction of isocrinids to the deep-sea settings may have occurred at the end of the Eocene around Antarctica and Australia, and later in the early Miocene in New Zealand. Here, we report the anomalous occurrence of the isocrinids in shallow nearshore marine facies from the middle Miocene of Poland (Northern Hemisphere, Central Paratethys). Thus, globally, this is the youngest record of shallow-sea stalked crinoids. This finding suggests that some relict stalked crinoids may have been able to live in the shallow-water environments by the middle Miocene, and further confirms that the depth restriction of isocrinids to offshore environments was not synchronous on a global scale.

Indexed as

Aquatic OrganismsFossilsAnimalsBiological EvolutionOceans and SeasPaleontologyCenozoicEchinodermsNeogenePredationSea lilies

Identifiers

PMID39095508
PMCPMC11297034

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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.