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首页> 外文期刊>Journal of Crustacean Biology >A NEW HOMOLODROMIOID CRAB (BRACHYURA: DROMIACEA: TANIDROMITIDAE) FROM THE BAJOCIAN OF CENTRAL POLAND AND A REVIEW OF THE STRATIGRAPHICAL DISTRIBUTION AND PALEOENVIRONMENTS OF THE KNOWN MIDDLE JURASSIC HOMOLODROMIOIDS
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A NEW HOMOLODROMIOID CRAB (BRACHYURA: DROMIACEA: TANIDROMITIDAE) FROM THE BAJOCIAN OF CENTRAL POLAND AND A REVIEW OF THE STRATIGRAPHICAL DISTRIBUTION AND PALEOENVIRONMENTS OF THE KNOWN MIDDLE JURASSIC HOMOLODROMIOIDS

机译:波兰中部巴约人的一种新的类汗蟹(Brachyura:Dromiacea:tanidromitidae)以及已知的中侏罗纪类人猿的地层分布和古环境综述

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A new homolodromioid (Brachyura, Tanidromitidae) crab from the Middle Jurassic (uppermost Bajocian) of central Poland is described and a new species, Tanidromites muelleri, is erected. The new species is not only one of the oldest representatives of true crabs, but also the most numerous in the world in terms of collected individuals (46 carapaces, including incomplete specimens) of the Middle Jurassic homolodromioid crabs. Tanidromites muelleri sp. nov. lived in a shallow-water, soft-bottom marine environment around developing oyster patch-reefs, being similar as later during the Late Jurassic when they lived in association with extensive sponge bioherms and coral reefs. The preservation of carapaces of the new species was influenced by a quick burial and rapid mineralization of calcitic concretions in which they are embedded. The stratigraphic distribution, to ammonite subzone level, of homolodromioid Middle Jurassic crabs is reviewed. Analysis of their paleoenvironmental preferences indicated that during the first step in the origin of true crabs they were connected with shallow, marine, high-energy carbonate deposits dominated by oolitic (including ferrugineus-oolitic one) facies, coralliferous reefs, and grey/black clays with carbonate concretions which hosted these crabs.
机译:描述了一种来自波兰中部侏罗纪中部(最上端的巴约西亚人)的新同绒螯蟹(Brachyura,Tanidromitidae)蟹,并建立了一个新的物种Tanidromites muelleri。新物种不仅是真蟹的最古老的代表之一,而且在中侏罗纪同绒螯蟹的个体(46个甲壳,包括不完整的标本)方面也是世界上最多的代表。 Tanidromites muelleri sp。十一月居住在发育中的牡蛎礁周围的浅水,软底海洋环境中,与后来的侏罗纪时期相似,它们与大量的海绵生物礁和珊瑚礁生活在一起。新物种的甲壳虫的保存受到埋葬它们的钙质固结物的快速埋葬和快速矿化的影响。综述了同侏罗纪中侏罗统螃蟹的地层分布,直至亚sub子水平。对古环境偏好的分析表明,在真蟹起源的第一步中,它们与浅,海洋,高能的碳酸盐矿床有关,这些矿床主要由橄榄岩(包括铁水成岩的)相,珊瑚礁和灰色/黑色黏土为主含有这些螃蟹的碳酸盐结石。

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