Pj. Markwick, Crocodilian diversity in space and time: the role of climate in paleoecology and its implication for understanding K/T extinctions, PALEOBIOL, 24(4), 1998, pp. 470-497
The taxonomic diversity of crocodilians (Crocodylia) through the last 100 m
illion years shows a general decline in the number of genera and species to
the present day. But this masks a more complex pattern. This is investigat
ed here using a comprehensive database of fossil crocodilians that provides
the opportunity to examine spatial and temporal trends, the influence of s
ampling, and the role of climate in regulating biodiversity.
Crown-group crocodilians, comprising the extant families Alligatoridae, Cro
codylidae and Gavialidae, show the following trend: an initial exponential
diversification through the Late Cretaceous and Paleocene that is restricte
d to the Northern Hemisphere until after the K/T boundary; relatively const
ant diversity from the Paleocene into the middle Eocene that may be an arti
fact of sampling, which might mask an actual decline in numbers; low divers
ity during the late Eocene and Oligocene; a second exponential diversificat
ion during the Miocene and leveling off in the late Miocene and Pliocene; a
nd a precipitous drop in the Pleistocene and Recent. The coincidence of dro
ps in diversity with global cooling is suggestive of a causal link-during t
he initial glaciation of Antarctica in the Eocene and Oligocene and the Nor
thern Hemisphere glaciation at the end of the Pliocene. However, matters ar
e complicated in the Northern Hemisphere by the climatic effects of regiona
l uplift.
Although the global trend of diversification is unperturbed at the K/T boun
dary, this is largely due to the exceptionally high rate of origination in
the early Paleocene. Nonetheless, the survival of such a demonstrably clima
te-sensitive group strongly suggests that a climatic explanation for the K/
T mass extinctions, especially the demise of the dinosaurs, must be reconsi
dered.