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华北克拉通河南西部寒武纪叠层石的形态与环境多样性

Morphological and environmental varieties of the Cambrian stromatolites in Western Henan, North China Craton.

作者信息

Chang Yu-Guang, Qing Shi-Yun, Dai Ming-Yue, Chen Song-Hua

机构信息

Henan Polytechnic University, Jiaozuo, Henan, China.

出版信息

PLoS One. 2025 Mar 28;20(3):e0319713. doi: 10.1371/journal.pone.0319713. eCollection 2025.

Abstract

Morphological varieties of Cambrian stromatolites in western Henan, North China Craton were essentially related to palaeoenvironmental parameter changes of the marine-floor. Small plexiform, hemispherical-smooth wavy, small columnar, irregular small columnar stromatolites, and stromatolites that surrounding flat-pebble conglomerate limestones are identified, in which the last type of stromatolite is unique, and they possess different macromorphology and micromorphology characteristics. A large number of Girvanella fossils, which were distributed in prostrate or horizontal and winding or overlapping patterns, were preserved in the laminae of stromatolites, and the dark laminae were formed by combined effect of Girvanella and precipitation of calcium carbonate. The research elucidates that small plexiform and small columnar stromatolite developed in the supratidal zone, hemispherical-smooth wavy, small columnar stromatolites, and stromatolites that surrounding flat-pebble conglomerate limestones grew in the intertidal zone with weaker hydrodynamic conditions, as well as irregular small columnar stromatolites occurred in subtidal zone. The features of microscopic laminae of stromatolites are influenced by microorganisms and metazoan, the macroscopic morphologies and growth of stromatolites are affected and controlled by terrigenous materials, hydrodynamic conditions and sedimentary substrates.

摘要

华北克拉通河南西部寒武纪叠层石的形态多样,主要与海底古环境参数变化有关。识别出了小型丛状、半球形-光滑波状、小型柱状、不规则小型柱状叠层石,以及围绕扁平砾石砾岩灰岩的叠层石,其中最后一种叠层石较为独特,它们具有不同的宏观形态和微观形态特征。大量以平卧或水平、蜿蜒或重叠模式分布的吉万藻化石保存在叠层石的纹层中,深色纹层是吉万藻与碳酸钙沉淀共同作用形成的。研究表明,小型丛状和小型柱状叠层石发育于潮上带,半球形-光滑波状、小型柱状叠层石以及围绕扁平砾石砾岩灰岩的叠层石生长于水动力条件较弱的潮间带,不规则小型柱状叠层石出现在潮下带。叠层石微观纹层特征受微生物和后生动物影响,其宏观形态和生长受陆源物质、水动力条件和沉积基底的影响与控制。

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