在亚洲东北部permi地区,双壳软体动物的寿命和繁殖速度

A. S. Biakov
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本文讨论了东北亚二叠纪双壳类物种和属的生存时间和形成速度。已经确定,该物种平均存在了2-5百万年;而这个属,持续了一千万年到两千万年。绝大多数长寿的分类群是早二叠世(亚塞利亚-中阿廷斯基)组合的特征。超过1000万年的长寿物种的比例超过了这一阶段存在的所有双壳类物种的25%。自阿廷斯基纪结束以来(自昆古里纪以来更是如此),相对短命物种的数量显著增加。造成这一现象的可能原因可能是由于地球内源活动的增加,导致地球生物圈以灭绝(Biakov, 2012a)事件的表现频率增加,并表现为各种性质的火山活动和深部流体对生物群的影响。一个覆盖了几乎整个下二叠世、以地质历史相对平静为特征的长时间间隔,被一个剧烈动荡的间隔所取代,这也影响了包括双壳类在内的整个生物群的发育。类群形成的速度也与地球生物圈事件有关,并主要受灭绝事件控制。
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Продолжительность существования и скорость образования видов и родов двустворчатых моллюсков в перми Северо-Востока Азии
The article discussed the duration of existence and the rate of formation for Permian bivalve species and genera in Northeast Asia. It has been established that the species existed averagely for 2-5 million years; and the genera, for 10-20 million years. The vast majority of long-lived taxa characterize the Early Permian (Asselian-Middle Artinskian) assemblages. The proportion of long-lived species that existed for over 10 million years exceeds 25 % of all bivalve species existing on this stage. Since the end of the Artinskian (and even more so since the Kungurian), the number of relatively short-lived species increased significantly. The possible reason for this phenomenon might have been an increase in the frequency of manifestation of geobiospheric, mainly extinction (Biakov, 2012a), events, resulted from an increase in the Earth endogenous activity, and expressed in the manifestation of volcanic activity of various nature and the deep fluids impact on the biota. A long time interval, covering almost the entire Lower Permian and characterized by a relatively calm course of geological history, was replaced by an interval with sharp upheavals manifested, which also affected the development of the entire biota, including bivalves. The rate of taxa formation is also associated with geobiospheric events and is controlled primarily by extinction events.
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