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Longjiangdong Coral Reef Palaeoecology of the Upper Carboniferous Huanglong Formation in Tianlin County, Guangxi Province[J]. Acta Sedimentologica Sinica, 2013, 31(3): 404-412.
Citation: Longjiangdong Coral Reef Palaeoecology of the Upper Carboniferous Huanglong Formation in Tianlin County, Guangxi Province[J]. Acta Sedimentologica Sinica, 2013, 31(3): 404-412.

Longjiangdong Coral Reef Palaeoecology of the Upper Carboniferous Huanglong Formation in Tianlin County, Guangxi Province

  • Publish Date: 2013-06-10
  •  A Late Carboniferous coral frame reef developes in Longjiangdong village, Tianlin County, Guangxi Province. The reef basing on the crinoid fragments beach has three separate cycles. The reefbuilder is the fasciculate Diphyphyllum sp. and the reefadherers mainly are crinoids, brachiopods, some kinds of algaes and foraminifers. Reefbuilding communities which just commonly grow together are lack of longterm, stable, complex ecological relationships. The maturity of reef biomes is poor and other reefbuilding ways are absence except Diphyphyllum sp. building the frame. It is formatted only immature stratigraphic reef under polytropic hydrodynamic conditions. The reasons why the Longjiangdong coral reef express such a distinctive characteristic are summarized as the following: the impacts of global geological structure changes in the Middle Carboniferous, the effects of microfloras and algaes in reefbuilding are not obvious, the benthic community is suppressed by crinoids, the reefbuilding capacity of Diphyphyllum sp. is poor for its ecological characteristics.
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    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 3.7 %FULLTEXT: 3.7 %META: 88.5 %META: 88.5 %PDF: 7.8 %PDF: 7.8 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 5.5 %其他: 5.5 %其他: 2.3 %其他: 2.3 %China: 0.5 %China: 0.5 %San Jose: 0.5 %San Jose: 0.5 %United States: 1.8 %United States: 1.8 %东莞: 0.5 %东莞: 0.5 %中卫: 0.5 %中卫: 0.5 %兰州: 0.5 %兰州: 0.5 %凉山: 0.5 %凉山: 0.5 %北京: 15.6 %北京: 15.6 %南宁: 0.5 %南宁: 0.5 %台州: 0.9 %台州: 0.9 %哥伦布: 0.5 %哥伦布: 0.5 %山景城: 0.5 %山景城: 0.5 %广州: 0.5 %广州: 0.5 %张家口: 1.8 %张家口: 1.8 %成都: 0.9 %成都: 0.9 %杭州: 0.9 %杭州: 0.9 %深圳: 1.8 %深圳: 1.8 %湖州: 0.9 %湖州: 0.9 %漯河: 0.5 %漯河: 0.5 %芒廷维尤: 20.6 %芒廷维尤: 20.6 %苏州: 0.9 %苏州: 0.9 %衢州: 0.5 %衢州: 0.5 %西宁: 39.4 %西宁: 39.4 %长沙: 0.5 %长沙: 0.5 %青岛: 0.5 %青岛: 0.5 %其他其他ChinaSan JoseUnited States东莞中卫兰州凉山北京南宁台州哥伦布山景城广州张家口成都杭州深圳湖州漯河芒廷维尤苏州衢州西宁长沙青岛
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Published:  2013-06-10

Longjiangdong Coral Reef Palaeoecology of the Upper Carboniferous Huanglong Formation in Tianlin County, Guangxi Province

Abstract:  A Late Carboniferous coral frame reef developes in Longjiangdong village, Tianlin County, Guangxi Province. The reef basing on the crinoid fragments beach has three separate cycles. The reefbuilder is the fasciculate Diphyphyllum sp. and the reefadherers mainly are crinoids, brachiopods, some kinds of algaes and foraminifers. Reefbuilding communities which just commonly grow together are lack of longterm, stable, complex ecological relationships. The maturity of reef biomes is poor and other reefbuilding ways are absence except Diphyphyllum sp. building the frame. It is formatted only immature stratigraphic reef under polytropic hydrodynamic conditions. The reasons why the Longjiangdong coral reef express such a distinctive characteristic are summarized as the following: the impacts of global geological structure changes in the Middle Carboniferous, the effects of microfloras and algaes in reefbuilding are not obvious, the benthic community is suppressed by crinoids, the reefbuilding capacity of Diphyphyllum sp. is poor for its ecological characteristics.

Longjiangdong Coral Reef Palaeoecology of the Upper Carboniferous Huanglong Formation in Tianlin County, Guangxi Province[J]. Acta Sedimentologica Sinica, 2013, 31(3): 404-412.
Citation: Longjiangdong Coral Reef Palaeoecology of the Upper Carboniferous Huanglong Formation in Tianlin County, Guangxi Province[J]. Acta Sedimentologica Sinica, 2013, 31(3): 404-412.

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