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JOURNAL ARTICLE
A Cretaceous-Tertiary Mass Extinction?
John C. Briggs
BioScience
Vol. 41, No. 9 (Oct., 1991), pp. 619-624 (6 pages)
Published by: Oxford University Press on behalf of the American Institute of Biological Sciences
https://www.jstor.org/stable/1311699
科学家然后开始研究热带的shadow-water里面marine 动物的灭绝,发现热带海水里的灭绝率高于其他地区,并导致了在此灭绝之后,热带海水里的动物存留下来的都是primitive的。
Among the marine plankton species, it was the smaller, more generalized, or primitive forms that survived the extinction, whereas the large, specialized species died out (Keller 1989, Lipps 1986). The generalized species lived in the cooler waters of high latitudes and, when the tropical species were eliminated, the primitive forms moved toward the equator to take their places (Gerstel et al. 1986). In other marine groups with good fossil records, such as the hermatypic corals (Stehli and Wells 1971), hivalve molluscs (Hecht and Agan 1972), and benthic foraminiferans (Durazzi and Stehli 1973), the younger more advanced genera are found in the tropics, whereas the more ancient genera were found at higher latitudes. In other groups, such as fishes and cetaceans, whose fossil history is not as well known, the higher-latitude representatives often have a simpler, more primitive morphology.
The K/T extinctions preferentially eliminated the tropical shelf and epipelagic organisms. This set of extinctions created an ecological vacuum, which was gradually populated by simpler, eurythermic organisms from higher latitudes and possibly from deeper water and other refuges. I have suggested that this process of succession by older, more primitive forms set back the evolutionary clock to an earlier time (Briggs 1990). So, instead of evolutionary benefits, the K/T extinctions resulted in evolutionary disaster. Depending on the habitat, it took the marine world from 3 million years to more than 25 million years to recover its late Cretaceous diversity.
文章中说首先很多人都将白垩纪生物灭绝的重点放在extinction of dinosaurs, 然后发现恐龙的灭绝既不是sudden也不是catastrophic, 而是逐渐灭绝的,尤其是在最后的3000年内。 The fossils have an interesting story to tell about the time over which the K/T extinctions took place, even though it is less spectacular than most current accounts. In both the marine and terrestrial environments, extinctions in major groups of animals began several million years before the K/T boundary. For example, the ammonites began to die out approximately 6 million years before and the dinosaurs approximately 7 million years before. In the shallow, tropical marine waters, where the majority of the extinctions took place, the macroinvertebrates died out over a 2.50—2.75 million year interval. The pelagic plankton species that disappeared did so over a shorter time, but their demise still took place over a period of 0.8-1.0 million years. These changes were certainly not sudden nor catastrophic.
3、highlight那段关于1%的
说明了海洋生物的灭绝对物种多样性的影响
The magnitude of the K/T extinctions has been consistently exaggerated. Recent estimates range from a kill of half the species on Earth on up to 80%. Such estimates have no scientific basis. Some 98% of living species belong to groups (terrestrial arthropods, vascular plants, and nematodes) for which we have virtually no extinction information. They may have passed through the K/T boundary relatively unscathed. Most of the high-latitude and deep-water marine groups lost relatively few species. The loss of species diversity on a global basis could have been less than 1%.
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