Impacts and marine invertebrate extinctions

@article{Macleod1998ImpactsAM,
  title={Impacts and marine invertebrate extinctions},
  author={N Macleod},
  journal={Geological Society, London, Special Publications},
  year={1998},
  volume={140},
  pages={217 - 246}
}
  • N. Macleod
  • Published 1998
  • Geography, Environmental Science
  • Geological Society, London, Special Publications
Abstract The Phanerozoic history of life has been interrupted by at least 17 different stage-level episodes of elevated extinction intensity. These range from major turnovers that affected the majority of the Earth’s extant biota (e.g. the Tatarian, Ashgill, and Maastrichtian events) to much smaller and perhaps more geographically localized disruptions. Review of available stage-level stratigraphic evidence suggests that bolide impacts do not exhibit a compelling correspondence to the… 

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References

SHOWING 1-10 OF 283 REFERENCES
Flood basalts and extinction events
The largest known effusive eruptions during the Cenozoic and Mesozoic Eras, the voluminous flood basalts, have long been suspected as being associated with major extinctions of biotic species.
Extinction and survivorship of southern Tethyan Benthic foraminifera across the Cretaceous/Palaeogene boundary
Abstract The benthic foraminiferal record from the Cretaceous/Palaeogene boundary stratotype of El Kef, Tunisia, shows a succession of three distinct assemblages. The late Maastrichtian upper bathyal
Biogeography of cretaceous/tertiary (k/t) planktic foraminifera
As a result of the process‐level connections between biogeography, systematics, and ecology, analyses of the spatial distribution of organisms across major extinction events can be used to probe the
Permo-Triassic Extinctions: Relation to Sea-Floor Spreading
  • T. Schopf
  • Environmental Science, Geography
    The Journal of Geology
  • 1974
An analysis of the Permo-Triassic fauna and paleogeography on a stage-by-stage basis supports previous more general summaries by concluding that the number of families of marine invertebrates was
Background and Mass Extinctions: The Alternation of Macroevolutionary Regimes
Comparison of evolutionary patterns among Late Cretaceous marine bivalves and gastropods during times of normal, background levels of extinction and during the end-Cretaceous mass extinction
The biology of mass extinction: a palaeontological view.
  • D. Jablonski
  • Environmental Science, Geography
    Philosophical transactions of the Royal Society of London. Series B, Biological sciences
  • 1989
TLDR
Taxa and adaptations can be lost not because they were poorly adapted by the standards of the background processes that constitute the bulk of geological time, but because they lacked--or were not linked to--the organismic, species-level or clade-level traits favoured under mass-extinction conditions.
The case for sea-level change as a dominant causal factor in mass extinction of marine invertebrates
  • A. Hallam
  • Environmental Science, Geography
  • 1989
A correlation between global marine regressions and mass extinctions has been recognized since the last century and received explicit formulation, in a model involving habitat-area restriction, by
Ammonoid extinction events
The ammonoid cephalopods range from the early Devonian to the late Cretaceous, a period of some 320 Ma. Because of their importance for biostratigraphic discrimination and their use in practical age
Taxonomic selectivity and continuous variation in mass and background extinctions of marine taxa
TLDR
It is shown that except for the late Permian event, mass-extinction rates for each taxon were often not higher than many of their 'normal' background rates evincing continuous variation between them.
The Cretaceous-Tertiary biotic transition
Mass extinctions are recognized through the study of fossil groups across event horizons, and from analyses of long-term trends in taxonomic richness and diversity. Both approaches have inherent
...
...