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Agglutinated foraminifera and sequence stratigraphy from the Chipaque Formation (Upper Cretaceous) of El Crucero section, Colombia, South America

机译:南美洲哥伦比亚埃尔克鲁塞罗地区奇帕克组(上白垩统)的有孔有孔虫和层序地层

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摘要

Agglutinated foraminifera from a section of the Chipaque Formation (Cenomanian-Campanian) in the Eastern Cordillera of Colombia are reported. The foraminiferal assemblage is dominated by species of the genera Ammobaculites and Haplophragmoides. The stratigraphic ranges of Ammobaculites colombianus, Haplophragmoides walteri, and Haplophragmoides rugosus are extended from a previously known Coniacian-Maastrichtian to a Cenomanian-Maastrichtian distribution, according to their appearance in the Chipaque Formation. Similarly, the range of Saccamina globosa (Cenomanian-Turonian) is extended to the Maastrichtian. The predominance of agglutinated foraminifera in the section is ascribed to undersaturation of calcium carbonate in the water column over the inner to outer shelf, due to the influx of terrigenous material. The array of parasequences composed of mudstone-sandstone couplets indicate landward and basinward coastline migrations that correspond to third order depositional sequences.
机译:据报道,哥伦比亚东部山脉的奇帕克地层(西诺曼尼亚-坎帕尼亚)的一部分有孔虫。有孔虫的组合主要由烟粉虱和单翅目属的物种主导。根据其在奇帕克组中的出现,哥伦比亚的弹药,Haplophragmoides walteri和Haplophragmoides rugosus的地层范围从先前已知的柯尼西亚-马斯特里赫特分布扩展到塞诺曼尼亚-马斯特里赫特分布。同样,萨卡米纳球菌(西诺曼尼亚语-土耳其语)的范围也扩大到了马斯特里赫特语。该部分中有孔虫的凝集主要是由于陆源物质的涌入,导致水柱内外架子上碳酸钙的饱和度不足。由泥岩-砂岩couple联组成的副层序阵列表明陆上和盆地向海岸线的迁移与三阶沉积层序相对应。

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