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Implemention of IGES-based CAD/CMM automatic workpiece modelling 基于iges的CAD/CMM自动工件建模的实现
Pub Date : 2000-01-01 DOI: 10.3969/j.issn.1003-5451.2000.03.007
Z. Zuo, S. Liiu, Xinhui Ma
The largest extinction in Earth history, in the latest Permian, was followed throughout most of the Early Triassic by a prolonged period of ecologic recovery. What factors delayed biotic recovery are still under debate and partly revolve around impacts of global warming on primary marine productivity. We examined N isotope records from the Festningen section on Spitsbergen to examine changes in nutrient availability through the Early to Middle Triassic along the northern margin of Pangea. Our results show progressive decline in N availability throughout the Griesbachian, leading to severe nutrient limitations through the remainder of the Early Triassic, until returning to a highly productive continental margin in Middle Triassic time. These results are consistent with other studies from northern and western Pangea and thus show regional nutrient limitations occurred in what should have been the main zone of marine primary productivity. Such nutrient limitation likely stressed primary production and consequently contributed to prolonged marine recovery. We suggest this was driven by high ocean temperatures depressing the marine nutricline.
地球历史上最大规模的物种灭绝发生在二叠纪晚期,随后在早三叠纪的大部分时间里,出现了一段漫长的生态恢复期。究竟是什么因素延迟了生物的恢复仍在争论中,部分围绕着全球变暖对初级海洋生产力的影响。我们研究了斯匹次卑尔根岛Festningen剖面的N同位素记录,以研究盘古大陆北缘早至中三叠世营养物质有效性的变化。我们的研究结果表明,整个Griesbachian的氮有效性逐渐下降,导致早三叠世剩余时间内严重的营养限制,直到中三叠世时期恢复到高产的大陆边缘。这些结果与盘古大陆北部和西部的其他研究结果一致,因此表明区域营养限制发生在本应是海洋初级生产力的主要区域。这种营养限制很可能对初级生产造成压力,从而导致海洋恢复时间延长。我们认为这是由于海洋高温抑制了海洋营养线。
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航空精密制造技术
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