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Geological duration of ammonoids controlled their geographical range of fossil distribution

机译:铵盐的地质持续时间控制着其化石分布的地理范围

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摘要

The latitudinal distributions in Devonian–Cretaceous ammonoids were analyzed at the genus level, and were compared with the hatchling sizes (i.e., ammonitella diameters) and the geological durations. The results show that (1) length of temporal ranges of ammonoids effected broader ranges of fossil distribution and paleobiogeography of ammonoids, and (2) the hatchling size was not related to the geographical range of fossil distribution of ammonoids. Reducing the influence of geological duration in this analysis implies that hatchling size was one of the controlling factors that determined the distribution of ammonoid habitats at any given period in time: ammonoids with smaller hatchling sizes tended to have broader ammonoid habitat ranges. These relationships were somewhat blurred in the Devonian, Carboniferous, Triassic, and Jurassic, which is possibly due to (1) the course of development of a reproductive strategy with smaller hatchling sizes in the Devonian and (2) the high origination rates after the mass extinction events.
机译:在属水平上分析了泥盆纪-白垩纪铵盐的纬度分布,并与孵化的大小(即铵盐直径)和地质持续时间进行了比较。结果表明:(1)铵盐的时间范围的长度影响了更广泛的铵盐化石分布和古生物地理范围;(2)孵化的大小与铵盐化石分布的地理范围无关。在此分析中减少地质持续时间的影响意味着,在任何给定的时间段内,孵化规模是决定氨类动物栖息地分布的控制因素之一:孵化规模较小的氨类动物倾向于具有更宽的氨类动物栖息地范围。在泥盆纪,石炭纪,三叠纪和侏罗纪,这些关系有些模糊,这可能是由于(1)泥盆纪的孵化规模较小的生殖策略的发展过程和(2)大规模成虫后的高起源率灭绝事件。

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