K/T Impact: support from an analysis of recovry and productivity!

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carlosMM

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Faunal evidence for reduced productivity and uncoordinated recovery in Southern Hemisphere Cretaceous-Paleogene boundary sections

Martin Aberhan1, , Sven Weidemeyer1, Wolfgang Kiessling1, Roberto A. Scasso2, Francisco A. Medina2

1. Museum für Naturkunde, Humboldt-Universität Berlin, Invalidenstrasse 43, D-10115 Berlin, Germany, 2. Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, 1428 Buenos Aires, Argentina

The mass extinction at the Cretaceous-Paleogene boundary is generally explained by a severe crisis in primary productivity, following a catastrophic bolide impact. Consistent with this scenario, Danian mollusk-dominated benthic shelf ecosystems of southern middle paleolatitudes (Neuquén Basin, Argentina) are characterized by (1) a stratigraphically limited low in macrofossil abundances; (2) an increase in starvation-resistant, nonplanktotrophic deposit feeders and chemosymbionts; (3) a reduction in the average body size of individuals; and (4) individuals with inactive lifestyles being more common than in the late Maastrichtian. Return to pre-extinction conditions of the various synecological attributes occurred over unequal time spans, indicating that recovery was uncoordinated with respect to ecological traits. Global comparison of ecological patterns suggests that reduced food supply (1) was a controlling factor in both hemispheres; (2) affected macrobenthic marine faunas at various distances from the Chicxulub impact site; and (3) was more effective in siliciclastic environments as compared to oligotrophic carbonate settings.

Keywords: mass extinction, Cretaceous-Paleogene boundary, ecology, productivity, Southern Hemisphere

Received: 14 July 2006; Revised: 10 October 2006; Accepted: 12 October 2006


Interesting! If anybody wants it I can get the PDF the next time I am in the office. Martin Aberhan is a cautious man, but the way I read the abstract it means that there really was a massive (I should rather say MASSIVE) disturbance of the food chain right at the K/T boundary. Mark another one for the impact theory!
 
Paleogene? So did they change the name from paleocene to paleogene after i got out of highschool?
 
*walks in thread*

makes attempt at understanding this

*walks out of thread*
 
Bast, TLC: I can't really go posting the full PDF here (copyright issue), but if you PM me your emails..... If you prefer not to do so, I'll see to it that I find a better solution.
 
Bleeping copyrights. Research should be free for all!
 
I know it is not related to the topic, but I read somwhere that the asteroid impact caused almost complete destruction of the ozone layer and it took decades before it recovered. How did the plants survive that?
 
I know it is not related to the topic, but I read somwhere that the asteroid impact caused almost complete destruction of the ozone layer and it took decades before it recovered. How did the plants survive that?

the K/T extinction occured over a period of 10,000 years. That it was caused by a meteorite is a sensationalist misconception.
 
Well, the impact triggered it.

What makes you say that? My understanding of the K/T extinction event (one of many throught the history of the Earth) was that it was bought about by changes in temprature in which certain species became progressively less adapted to the environment.

Also, the pattern of extinction is inconsistent with the effects of a meteroite impact at K/T.

Back me up boffins.
 
Cambrian, probably.
Carboniferous. Cambrian is Є.
But T stands for Triassic in the P/T boundary, if they can reuse it for tertiary why not the C?

The Triassic used to be a "Tr" ligature. With the demise of the Tertiary as a formally recognized unit, the simple T appears to've quietly reattached itselt to the Triassic.
 
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