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UPPER TRIASSIC CALCAREOUS ALGAE FROM THE PANTHALASSA OCEAN

机译:来自巅峰的泛达颅钙藻类海洋

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Upper Triassic calcareous algae, abundant and well-diversified in Tethyan deposits, have rarely been described in rocks of Panthalassan origin. Over the past ten years, several studies were performed on Upper Triassic carbonate deposits of Panthalassan affinity in North America, Japan and Far East Russia, revealing unexpectedly rich and diversified assemblages. The samples were collected from nine localities situated on both sides of the Pacific Ocean. The identified algal assemblage consists of green and red algae, including fourteen dasycladaleans, rare bryopsidaleans, and several rhodophyceans. This paper describes the main algal taxa, including six new species: Holosporella? rossanae Bucur & Del Piero n. sp., Holosporella magna Bucur & Fucelli n. sp., Griphoporella minuta Bucur & Peybernes n. sp., Patruliuspora pacifica Bucur, Del Piero & Peyrotty n. sp., Patruliuspora oregonica Bucur & Rigaud n. sp. and Collarecodium? nezpercae Bucur & Rigaud n. sp. Rivulariacean-like cyanobacteria and thaumatoporellacean algae are also present. The whole Panthalassan algal assemblage comprises both unknown (?endemic) and common taxa of the Tethyan domain. To explain the cosmopolitan distribution of various Upper Triassic benthic organisms (scleractinian corals, calcified sponges, foraminifera), a close connection with the Tethys Ocean was hypothesized by different authors. During the Late Triassic, the Tethys was open to the east on the Western Panthalassa but not to the west, suggesting that Triassic calcareous algae were able to efficiently colonize environments that are estimated to be more than 10'000 km apart. An adventitious transport of calcareous algae and/or their spores is proposed to explain this long-range algal dispersal.
机译:上三叠纪钙质藻类,在岩岩山的岩石中充足,丰富多样化,很少被描述为巅峰的巅峰。在过去的十年中,在北美,日本和远东俄罗斯蓬桑萨氏族亲和力的上三叠系碳酸盐矿床上进行了几项研究,揭示了意外丰富和多样化的集会。从太平洋两侧的九个地方收集样品。鉴定的藻类组合包括绿色和红藻类,包括十四次达斯Ycladaleans,罕见的Bryopsidals和几种肾小序。本文介绍了主要的藻类分类群,包括六种新种:Holosporella? rossanae bucur&del piero n。 SP。,Holosporella Magna Bucur&Fucelli n。 SP。,格列皮别墅Minuta Bucur&Peybernes n。 SP。,Partuliuspora Pacifica Bucur,Del Piero&Peytotty n。 SP。,Patrulutiuspora oregonica Bucur&Rigaud n。 SP。和锁骨? Nezpercae Bucur&Rigaud n。 SP。还存在RivulariaceAn样的蓝藻和硫咖啡素藻类。整个披肩藻类组合包括未知(?地方)和Tethyan结构域的常见分类。为解释各种上三叠系底栖生物的多溴聚发作(Scleractinian珊瑚,钙化海绵,Foraminifera),与Thethys海洋的密切连接由不同的作者假设。在迟到的三叠系中,特提斯在西部巅峰的东部开放,但不向西方开放,这表明三叠纪的钙质藻类能够有效地殖民,估计分开超过10000公里。提出了一种偶然的钙质藻类和/或其孢子的运输,以解释这种远程藻类分散。

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