| 相对海平面变化对腕足动物群落取代的影响——以吐哈盆地北缘桃西沟上石炭统祁家沟组—奥尔土组剖面为例 |
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| 引用本文： | 高金汉,王训练,傅国斌,宋健兴,秦恩鹏.相对海平面变化对腕足动物群落取代的影响——以吐哈盆地北缘桃西沟上石炭统祁家沟组—奥尔土组剖面为例[J].现代地质,2004,18(3):290-296. |
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| 作者姓名： | 高金汉 王训练 傅国斌 宋健兴 秦恩鹏 |
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| 作者单位： | [1]新疆吐哈油田分公司勘探开发研究院，新疆哈密839009 [2]中国地质大学地球科学与资源学院，北京100083 |
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| 基金项目： | 国家科技部自然科技资源E-平台建设项目(K02146). |
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| 摘 要： | 相对海平面的升降变化引起的相对水深及相关生态条件的改变对腕足动物群具有影响。相对海平面变化的速度和幅度是引起腕足动物群面貌变化的重要因素。相对海平面的持续缓慢上升有利于腕足动物丰度的增加和分异度的提高,海平面的大幅度快速变化对腕足动物群落则是一个不利的因素,是造成腕足动物物种丰度下降、新种增加量减少乃至彻底死亡的重要原因。吐哈盆地北缘晚石炭世发育的5个腕足动物群落全部与相对海平面上升期有关。在海平面的持续缓慢上升期,腕足动物的丰度不断增加,分异度迅速提高;而在相对海平面下降期,本区陆源粗碎屑物大量注入,不适合腕足动物的生存。
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| 关 键 词： | 晚石炭世 相对海平面变化 腕足动物 吐哈盆地 |
| 文章编号： | 1000-8527(2004)03-0290-07 |
| 修稿时间： | 2004年3月10日 |
THE INFLUENCE OF RELATIVE SEA LEVEL CHANGES TO THE REPLACEMENT OF BRACHIOPODS COMMUNITIES: A CASE STUDY OF TAOXIGOU CARBONIFEROUS SECTION OF THE NORTH MARGIN OF TURPAN-HAMI BASIN |
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| GAO Jin-han,WANG Xun-lian,FU Guo-bin,SONG Jian-xing,QIN En-peng.THE INFLUENCE OF RELATIVE SEA LEVEL CHANGES TO THE REPLACEMENT OF BRACHIOPODS COMMUNITIES: A CASE STUDY OF TAOXIGOU CARBONIFEROUS SECTION OF THE NORTH MARGIN OF TURPAN-HAMI BASIN[J].Geoscience——Journal of Graduate School,China University of Geosciences,2004,18(3):290-296. |
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| Authors: | GAO Jin-han WANG Xun-lian FU Guo-bin SONG Jian-xing QIN En-peng |
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| Institution: | GAO Jin-han~1,WANG Xun-lian~1,FU Guo-bin~2,SONG Jian-xing~2,QIN En-peng~2 |
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| Abstract: | Relative sea level change may result in the change of water depth and all the other ecological factors related, so it is a key factor for controlling the succession and replacement of brachiopods communities. The speed and extension of sea level rising and descending greatly control the species richness and diversity of brachiopods community. In the area of the north margin of Turpan-Hami basin, totally three third-order relative sea level changes can be recognized from the Upper Carboniferous, and all the 5 brachiopods communities developed during this period are closely related to the sea level risings. There is no brachiopods fossil found during the marine regression, this may result from the quick descending of relative sea level changes and too much clastic sediment swarmed into. During the period of sea level rising, the rapid rising of primary sea level is in favor of early brachiopods communities but may restrain the development of later comers. Constant and slow rising of sea level is helpful to the flourish of the species richness and diversity of brachiopods, but may delay the process of the replacement of brachiopods communities. |
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| Keywords: | Late Carboniferous relative sea level change brachiopods Turpan-Hami basin |
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