[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index][Subject Index][Author Index]
Early Triassic Marine Biotic Recovery
Another new paper:
http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0088987;jsessionid=D51520EFE466DC952C242885BED75637
Scheyer TM, Romano C, Jenks J, Bucher H (2014) Early Triassic Marine Biotic
Recovery: The Predators' Perspective. PLoS ONE 9(3): e88987.
doi:10.1371/journal.pone.0088987
Examining the geological past of our planet allows us to study
periods of severe climatic and biological crises and recoveries, biotic
and abiotic ecosystem fluctuations, and faunal and floral turnovers
through time. Furthermore, the recovery dynamics of large predators
provide a key for evaluation of the pattern and tempo of ecosystem
recovery because predators are interpreted to react most sensitively to
environmental turbulences. The end-Permian mass extinction was the most
severe crisis experienced by life on Earth, and the common paradigm
persists that the biotic recovery from the extinction event was
unusually slow and occurred in a step-wise manner, lasting up to eight
to nine million years well into the early Middle Triassic (Anisian) in
the oceans, and even longer in the terrestrial realm. Here we survey the global
distribution and size spectra of Early Triassic and Anisian
marine predatory vertebrates (fishes, amphibians and reptiles) to
elucidate the height of trophic pyramids in the aftermath of the
end-Permian event. The survey of body size was done by compiling maximum
standard lengths for the bony fishes and some cartilaginous fishes, and total
size (estimates) for the tetrapods. The distribution and size
spectra of the latter are difficult to assess because of preservation
artifacts and are thus mostly discussed qualitatively. The data
nevertheless demonstrate that no significant size increase of predators
is observable from the Early Triassic to the Anisian, as would be
expected from the prolonged and stepwise trophic recovery model. The
data further indicate that marine ecosystems characterized by multiple
trophic levels existed from the earliest Early Triassic onwards
guilds occurred less than two million years after the end-Permian extinction
event, in which a transition from fish/amphibian to
fish/reptile-dominated higher trophic levels within ecosystems became
apparent.