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The latest shallow-sea isocrinids from the Miocene of Paratethys and implications to the Mesozoic marine revolution.
Salamon, Mariusz A; Radwanska, Urszula; Paszcza, Karolina; Krajewski, Marcin; Brachaniec, Tomasz; Niedzwiedzki, Robert; Gorzelak, Przemyslaw.
Afiliación
  • Salamon MA; Faculty of Earth Sciences, Laboratory of Palaeontology and Stratigraphy, University of Silesia in Katowice, Bedzinska 60, 41-200, Sosnowiec, Poland.
  • Radwanska U; Faculty of Geology, Department of Historical, Regional Geology and Paleontology, University of Warsaw, Zwirki i Wigury93, 02-089, Warszawa, Poland.
  • Paszcza K; Faculty of Earth Sciences, Laboratory of Palaeontology and Stratigraphy, University of Silesia in Katowice, Bedzinska 60, 41-200, Sosnowiec, Poland.
  • Krajewski M; Doctoral School at the University of Silesia in Katowice, Bankowa 14, 40-007, Katowice, Poland.
  • Brachaniec T; Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059, Kraków, Poland.
  • Niedzwiedzki R; Faculty of Earth Sciences, Laboratory of Palaeontology and Stratigraphy, University of Silesia in Katowice, Bedzinska 60, 41-200, Sosnowiec, Poland.
  • Gorzelak P; Faculty of Earth Sciences and Environmental Management, Institute of Geological Sciences, Wroclaw University, Cybulskiego 30, 50-205, Wroclaw, Poland.
Sci Rep ; 14(1): 17932, 2024 08 02.
Article en En | MEDLINE | ID: mdl-39095508
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.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Organismos Acuáticos / Fósiles Límite: Animals Idioma: En Revista: Sci Rep Año: 2024 Tipo del documento: Article País de afiliación: Polonia

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Organismos Acuáticos / Fósiles Límite: Animals Idioma: En Revista: Sci Rep Año: 2024 Tipo del documento: Article País de afiliación: Polonia
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