about
The effect of geographic range on extinction risk during background and mass extinctionFormation of the Isthmus of PanamaClimate change and the selective signature of the Late Ordovician mass extinctionTwo-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunityClimate change and the past, present, and future of biotic interactions.Extinctions. Paleontological baselines for evaluating extinction risk in the modern oceans.The magnitude and duration of Late Ordovician-Early Silurian glaciation.Extinctions in ancient and modern seas.Marine extinction risk shaped by trait-environment interactions over 500 million years.Plate tectonic regulation of global marine animal diversity.Increase in predator-prey size ratios throughout the Phanerozoic history of marine ecosystems.The evolutionary consequences of oxygenic photosynthesis: a body size perspective.A signature of transience in bedrock river incision rates over timescales of 10(4)-10(7) years.Identifying the most surprising victims of mass extinction events: an example using Late Ordovician brachiopods.The Ordovician Radiation: A Follow-up to the Cambrian Explosion?Twelve thousand recent patellogastropods from a northeastern Pacific latitudinal gradient.Hierarchical complexity and the size limits of life.Quantifying the dark data in museum fossil collections as palaeontology undergoes a second digital revolutionIsotopes from fossil coronulid barnacle shells record evidence of migration in multiple Pleistocene whale populations
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description
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
Seth Finnegan
@ast
Seth Finnegan
@en
Seth Finnegan
@es
Seth Finnegan
@nl
type
label
Seth Finnegan
@ast
Seth Finnegan
@en
Seth Finnegan
@es
Seth Finnegan
@nl
prefLabel
Seth Finnegan
@ast
Seth Finnegan
@en
Seth Finnegan
@es
Seth Finnegan
@nl
P106
P21
P31
P496
0000-0002-6175-6173