Cited by 82Paleontology and Stratigraphy of FossilsEvolution and Paleontology StudiesPaleontology and Evolutionary Biology

The Ordovician chitinozoan biodiversification and its leading factors

Achab, Aïcha, Paris, Florentin·2007·Palaeogeography, Palaeoclimatology, Palaeoecology

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Crossref · 10.1016/j.palaeo.2006.02.030

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  • Even without sophisticated statistical methods, it is obvious that the global peaks of diversity are the sums of the peaks of regional diversity, as shown for several fossil groups such as chitinozoans.

    “Even without sophisticated statistical methods it is obvious that the global peaks of diversity are the sums of the peaks of regional diversity, as it has been clearly shown for several fossil groups, such as, for example, the chitinozoans (Paris et al., 2004; Achab and Paris, 2007), an example that should be followed by all other groups in the search for a true 'global ' biodiversity”

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Authors
Achab, A., & Paris, F.
Affiliations
Centre National de la Recherche Scientifique (FR)
Corresponding author
Paris, Florentin
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2007-03
Volume
245
Issue
1-2
Pages
5-19
ISSN
0031-0182 (ISSN-L)
OpenAlex
W2013847698
Cited by
82
References
49
Citations by year
2026: 2 · 2025: 2 · 2023: 7 · 2022: 4 · 2021: 4 · 2020: 3 · 2019: 9 · 2018: 4 · 2017: 4 · 2016: 3 · 2015: 4 · 2014: 3 · 2013: 3 · 2012: 5
FWCI
4.49
Type
journal article
Language
en
Open access
closed
Locations
  • Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion)
  • HAL (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
Keywords
Ordovician, Ordovician extinction, Laurentia, Baltica, northern Gondwana, endemism, thermohaline circulation, global cooling, Late Ordovician, Hirnantian glaciation

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