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Geosites of International Significance in the UNESCO WHS Lena Pillars Nature Park (Sakha Republic, Russia)

机译:联合国教科文组织世界人道主义峰会莉娜支柱自然公园(俄罗斯萨哈共和国)具有重要意义的地理位置

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The Lena Pillars Nature Park belonging to the Sakha Republic (Yakutiya) is situated in the southeastern Siberian Platform on the right bank of the middle Lena River. The park is mainly known for the almost continuous chain of fancy pillar-like carbonate weathering outliers spreading along the right bank of the Lena River and banks of its tributaries Botoma and Sinyaya. However, the main reason of the ultimate importance of the park is that it represents a pivotal evidence of relatively rapid evolutionary development and growth of the skeleton and soft-bodied fauna and algae diversity, which took place about 541–509Ma ago. This event is well known in the scientific world as the "Cambrian Explosion". The International Union of Nature Conservation included it into the list of key evolutionary events in the Earth's history. Numerous geosites of different types and significance levels are located in the park, and six of them are of international importance. They are highly representative in terms of stratigraphy, paleontology, paleoecology, and geomorphology. Stratigraphic geosites demonstrate nearly a continuous record of the Upper Ediacaran–Middle Cambrian deposits. Before the 1990s, stratotypes of the Lower Cambrian stages were used for standardization of the Lower Cambrian in the International Stratigraphic Chart. Paleontological geosites are mainly represented by fossil localities of the Early Cambrian, characterized by high level of preservation and diversity. Sinsk localities of the Early Cambrian biota are listed among the Cambrian Lagerst?ttens. Many geosites are objects of paleoecological investigations because their deposits were formed in synchronously existing parts of a former single paleobasin (inner lagoon, transitional reef, and outer abyssal) with different physical and chemical parameters. Geomorphologic sites represent different types of permafrost karst, as well as weathering outliers of columnar shape, the so-called Lena Pillars. The scientific and aesthetic value of the Lena Pillars Nature Park is globally recognized, and in 2012 it was inscribed into UNESCO WHL based on the criteria vii and viii.
机译:属于萨哈共和国(Yakutiya)的莉娜支柱自然公园位于莉娜河中游右岸的东南西伯利亚平台上。该公园主要因沿Lena河右岸及其支流Botoma和Sinyaya两岸分布的几乎连续的奇特的柱状碳酸盐风化异常点而闻名。然而,公园最终重要性的主要原因是它代表了大约541-509Ma以前骨骼和软体动物及藻类多样性相对较快的进化发展和增长的关键证据。该事件在科学界被称为“寒武纪爆炸”。国际自然保护联盟将其纳入地球历史上重要的进化事件清单。公园中有许多不同类型和重要程度的地理位置,其中六个具有国际重要性。它们在地层学,古生物学,古生态学和地貌学方面具有很高的代表性。地层地质站点几乎记录了上埃迪卡拉-中寒武纪沉积的连续记录。在1990年代之前,下寒武统阶段的地层型被用于国际地层图中的下寒武统。古生物学的地理位置主要以早寒武纪的化石为代表,其特征是高度的保存和多样性。寒武纪早期生物群的辛斯克地区被列为寒武纪拉格斯特山脉。许多地质遗迹是古生态研究的对象,因为它们的沉积物是在一个具有不同物理和化学参数的单一古古巴辛(内部泻湖,过渡礁和外部深渊)的同步存在的部分中形成的。地貌地貌代表了不同类型的永冻土喀斯特地貌,以及柱状形状的风化异常点,即所谓的Lena柱。莉娜柱子自然公园的科学和美学价值已得到全球认可,并在2012年根据vii和viii标准列入了联合国教科文组织世界遗产名录。

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