| [Thread Prev] | [Thread Next] | [Thread Index] | [Date Prev] | [Date Next] | [Date Index] |
Lest we forget, the impact winter is not the only environmental perturbation that organismal populations would have had to deal with. Acid rain (according to some scenarios think of automobile battery acid falling out of the sky) and global wildfires (by some accounts much of North America was burned to the ground) would also have played a role. So, in Neale's intriguing image, take that hedgehog (or beetle), dunk him in battery acid, then throw him on the barbie for (at least) a few hours, and then into the 'fridge for (at least) several months. For plants, add (at least) several months of twilight-levels of light penetration during the "day." Note also that if the June impact time is correct (Jack Wolfe's got at least a 1/12 chance of being right) this means that there would have been no summer that year (assuming the proximate effects lasted for only a few months) and that the winter would in all likelihood have been anomalously intense. Most papers dealing with the physical results of an impact argue that these effects would have played out over years, not months. Given this very approximate picture of a post-impact world we might ask whether the known pattern of terrestrial extinction and survivorship makes sense. Certainly the above scenario calls for extinctions to occur. But I think we should be trying for an explanation that says a bit more than "the K-T impact killed all the species all over the world, except for the ones it didn't kill." Dave Archibald has asked and provided preliminary answers to the question of comparing predictions and extinction patterns in a couple of recent publications. Archibald, J. D. 1996. Dinosaur extinction and the end of an era: what the fossils say. Columbia University Press, New York. Archibald, J. D., 1996. Testing extinction theories at the Cretaceous-Tertiary boundary using the vertebrate fossil record. In: MacLeod, N. & Keller, G. eds., The Cretaceous-Tertiary mass extinction: biotic and environmental changes. W. W. Norton & Co., New York, 373-398. I won't steal Dave's thunder by giving away his conclusions, but his analytical design and his results make very interesting reading. It is to these types of studies that we must turn to decide what role the K-T impact(s) may have played in the Late Cretaceous faunal transition. Even almost 20 years into this controversy, we've hardly scratched the surface of testing the biotic predictions of the various impact scenarios in any sort of detail. As the "K-T insect" string makes perfectly clear, there still a lot to be done in this area. Norm MacLeod ___________________________________________________________________ Dr. Norman MacLeod Micropalaeontological Research N.MacLeod@nhm.ac.uk (E-mail) Department of Palaeontology, The Natural History Museum, Cromwell Road, London, SW7 5BD Office Phone: 0171-938-9006 Dept. FAX: 0171-938-9277 E-mail: N.MacLeod@nhm.ac.uk ___________________________________________________________________
Partial index: