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The stratigraphic division and correlation of the Lower/Middle Cambrian boundary is a global problem that has not yet been solved even up to now. That is because there existed two distinctly different biogeographic regions during the Early and Middle Cambrian[1]—— the Indian-Pacific biogeographic region and the Atlantic biogeographic region. In the Atlantic biogeographic region the traditional Lower/Middle Cambrian boundary was marked by the extinction of Olenellids trilobite and the in… 相似文献
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关于喀斯特石漠和石漠化概念的讨论 总被引:48,自引:7,他引:48
喀斯特石漠化是近年来所认识到的一种地质生态灾害,所造成的经济、环境乃至社会影响越来越大,受到国家的广泛关注,但却存在生态建设超前、基础研究落后的严峻现实。本文总结了当前石漠化的类型划分和存在问题,从喀斯特生态系统运行的地学过程、生物学过程和人为过程出发,提出石漠化过程存在地质石漠化过程、生态系统石漠化过程和人为加速石漠化过程,对不同类型的石漠化宜分别采取保护、恢复、重建、维持措施。石漠和石漠化表达的时空范畴不同,是石漠化这一土地退化过程的最后或顶极结果,自然条件下其形成多与地表坡度较大有关,而人为加速石漠化过程中石漠化土地空间分布与地形坡度、地貌部位并无直接联系。建议以“干扰方式 植被 土壤 地貌”对人为加速石漠化过程导致的石漠化土地进行类型划分,评价的土地应分为非石漠化土地、行漠化土地和逆转优化的“基准化”土地。 相似文献
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埋藏条件下蒙脱石层间水的稳定性 总被引:3,自引:0,他引:3
王世杰 《矿物岩石地球化学通报》1998,(4)
蒙脱石族矿物广泛存在于地表各种环境中,其层间结构的稳定性对各种表生地质作用的发生和过程起着重要作用。在砂岩成岩作用中,蒙脱石族矿物的脱水作用改变了砂岩孔隙流体的量和成分,同时也降低了油气储蓄层的孔隙度和渗透性。泥、页岩中由于蒙脱石族矿物的脱水作用,在... 相似文献
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王世杰 《中国地球化学学报》1996,15(2):105-112
By using the improved trace(50μg) Sr isotope analytical method the ^87Sr/^86Sr ratios of Xiaodukou foraminifera fossils were measured,giving a range of 0.71105-0.71274,apparently higher than the value of contemporaneous seawater(0.709087-0.709147)and also slightly higher than the average value of modern Yellow River(0.7111),demonstrating that the contemporaneous environment where Xiaodukou foraminifera inhabited was an inland lake.Detailed analyses of △ Sr values showed that there occurred an event responsible for environmental changes in the ancient Nihewan Lake area during the time(about 1.0Ma ago)when Xiaodukou foraminifera appeared.Because of strong evaporation the salinity of the lake would increase and a regional salt-water of brackish-water lacustrine environment would be produced,thus providing a suitable and inhabitable environment for foraminiferae.It is concluded that Xiaodukou foraminiferal fossil assemblaes belong to non-marine foraminiferal species. 相似文献
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A global-scale glaciation occurred at about 600 Ma ago. As a result, the Earth became the “Snowball Earth“. The glaciation came to the end abruptly when atmospheric carbon dioxide increased to such an extent as to be about 350 times the modem level because of subaerial volcanic degassing. The rapid termination of glaciation would have led to warming of the Snowball Earth and extreme greenhouse conditions would have been created. The transfer of atmospheric carbon dioxide to oceans would give rise to the rapid precipitation of calcium carbonate in warm surface seawaters, thus forming the cap carbonate rocks as observed worldwide today. Regionally persisting, thin layers of carbonate rocks directly and ubiquitously overlie Proterozoic glacial deposits almost on every continent, and are commonly referred to as cap carbonates. Their unusual litho- fabrics, stratigraphically abrupt basal and upper-level contacts and strongly negative carbonate isotopic signatures ( δ ^13Cearb. values range from -7.0‰ —0‰) suggest a chemical oceanographic origin, the details of which remain unknown. It is proposed that these enigmatic deposits are related to the destabilization of gaseous hydrate in terrestrial permafrost following rapid postglacial warming and flooding of widely exposed continental shelves and internal basins. The authors carried out studies on the geochemistry, sedimentology and palacontology of the Sinian cap carbonates in Guizhou and Hunan provinces, including the occurrence of cap carbonates of unusual fabrics, strongly negative carbon isotopic signatures, and a lot of bitumen nodules.From the results it is suggested that the cap carbonates were formed from solid methane seepage, and it is in agreement with Kennedy‘‘ s viewpoint (2001) that the cap carbonates resulted from the rapid precipitation of calcium carbonate in response to solid methane seepage. 相似文献
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