Coevolution of Brachiopod Paleobiogeography and Tectonopaleogeography during the Early–Middle Permian
Coevolution of Brachiopod Paleobiogeography and Tectonopaleogeography during the Early–Middle Permian
复制标题
早、中二叠世腕足动物古生物地理学与构造古地理的共同演化
DOI：
10.1111/1755-6724.12598
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发表时间：
2015-12
期刊：
影响因子：
--
通讯作者：
李宁 （Lining）
中科院分区：
文献类型：
--
作者：
王成文（Wang Chengwen）;李宁 （Lining）
对已知早、中二叠世腕足动物区系进行综合整理和系统分析，发现早二叠世腕足动物区系由3界6区11省组成，中二叠世腕足动物区系由3界4区8省组成。通过对腕足动物区系格局的比较分析，揭示了早-中二叠世全球腕足动物古地理与构造古地理的共同演化。虽然温度/纬度是控制三界形成的主要因素，但构造古地理因素决定了大陆所在的温度/纬度。盘古大陆的“大陆屏障”作为一个“中轴线”大陆，将这三个领域划分为六个区域，这表明生物地理区域的形成主要受构造古地理因素的控制。构造古地理的演化有时是一个长期的过程，因此受构造古地理控制的生物地理区域（或省）表现出相对的稳定性。生物地理省的性质变化（如从冷水到温水，反之亦然）、地理范围的扩大或缩小以及部分省的重组都与区域构造演化有关。腕足动物古地理与构造古地理的协同演化研究不仅解释了早-中二叠世腕足动物古地理格局的形成机制，而且为该时期海洋和板块（块）的位置和配置提供了依据。
A comprehensive compilation and systematic analysis of known early and middle Permian brachiopod faunas shows that the early Permian brachiopod faunas comprise three realms, six regions, and eleven provinces, while those of the middle Permian comprise three realms, four regions, and eight provinces. A comparison and analysis of brachiopod faunal patterns reveal a coevolution between global brachiopod paleobiogeography and tectonopaleogeography during the early–middle Permian. Although temperature/latitude is the main factor controlling the formation of three realms, tectonopaleogeographic factors determine the temperature/latitude in which the continents were located. The ‘continental barrier’ of Pangea, as a ‘central axis’ continent, divided the three realms into six regions, which indicates that the formation of biogeographic regions was controlled mainly by the tectonopaleogeographic factors. The evolution of tectonopaleogeography was sometimes a long–term process, so that the biogeographic regions (or provinces) controlled by tectonopaleogeography displayed relative stability. Shifts in the nature of biogeographic provinces (e.g., from cool water to warm water, and vice versa), extensions or narrowing of geographical ranges, and recombinations of some provinces were all related to regional tectonic evolution. The study of the coevolution between brachiopod paleobiogeography and tectonopaleogeography not only accounts for the formation mechanisms of brachiopod paleobiogeographic patterns during the early–middle Permian, but also provides evidences for the locations and configurations of oceans and plates (blocks) during this period.
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影响因子：
0.9
作者：
J. Tazawa
通讯作者：
J. Tazawa
影响因子：
3.3
作者：
Liu Jianbo;Zhan Renbin
通讯作者：
Liu Jianbo;Zhan Renbin
DOI：
10.1111/j.1755-6724.2008.tb00319.x
发表时间：
2008-02
期刊：
Acta Geologica Sinica ‐ English Edition
影响因子：
--
作者：
J. Xiao-chi;Zhan Lipei
通讯作者：
J. Xiao-chi;Zhan Lipei
DOI：
10.1007/s11430-013-4670-x
发表时间：
2013-07
期刊：
Science China Earth Sciences
影响因子：
--
作者：
Chengwen Wang;GuoWei Zhao;Ning Li;P. Zong
通讯作者：
Chengwen Wang;GuoWei Zhao;Ning Li;P. Zong
影响因子：
3
作者：
M. Sone;Mohd. Shafeea Leman;G. Shi
通讯作者：
M. Sone;Mohd. Shafeea Leman;G. Shi