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机构地区:[1]中国科学院南京地质古生物研究所,南京210008 [2]广西大学海洋学院珊瑚礁研究中心,南宁530004 [3]北京大学地球与空间科学学院,北京100871
出 处:《古生物学报》2016年第3期314-326,共13页Acta Palaeontologica Sinica
基 金:科技部基础性项目(2013FY111000);国家自然科学基金委员会重大项目(41290260);国家自然科学重点基金(91428203);国家自科学基金(41173051)联合资助
摘 要:云南省昭通市东北郊箐门出露了一条比较完整的泥盆纪浅海相地层剖面,下、中、上三个统均有出露,浅海底栖生物化石丰富,研究基础也相对较好,是研究滇东北地区泥盆纪地层的一条理想剖面。由于地层剖面比较长,沉积厚度比较大,文中仅描述该剖面早泥盆世和中泥盆世早期的四射珊瑚,并讨论有关地层划分和珊瑚群古生物地理亲缘关系。The rugose corals described in the present paper were collected by one of the authors (Liao Weihua) from the Qingmen section of Zhaotong, NE Yunnan in 1972. These corals, occuring in association with brachiopods (Rostrospirifer ardenensis, Rostrospiri f er tonkinensis , Acrospiri f er orthogonalis, Acrospirifer lungmenshanensis, Atrypa sp., Cyrtina sp., "Delthyris" sp., Dicoelostrophia beblistriata , DicoeZostrophia punctata , Elyta sp., Eosophragmophora sp., Howittia sp., Howellella sp. , Kwangsia cf. yohi, Mesodouvillina orientalis, Nadiastrophia pattei, Parachonetes nasutus, Parathyrisina tangnae, Schuchertella sp. ), Stromatoporoids (Clathrodictyon sp., Anostylostroma sp. , Atelodictyon sp. , Ferestrom-atopora sp. ), and bivalves (Leptodesrna ? sp., Mytilarea sp. ), were found in a series of sandstones, mudstones intercalated with marls or argillaceous limestones. The rugose corals described and illustrated comprise 11 species within 8 genera. They include two rugose coral Assemblages in ascending order : The first rugose coral Assemblage (Early Devonian Emsian) :Acanthophyllum cf. guitangense Yu et Liao Australophyllum cyathophylloides Hill Calceola intermediata intermediata YohCalceola sandalina nanningensis Yoh Cystiphylloides cf. fongi (Yoh)Cystiphylloides mirabiLe Wedek:nd et Voll-brechtEdaphophyllum zhaotongense sp. nov. Tryplasma cf. guangxiensis Yu et Liao Xystriphyllum cf. The second rugose Devonian Eifelian) ; devonicum Bulvanker coral Assemblage (Middle Devonian Eifelian) ;Utaratuia yunnanensis sp. nov. X ystriphyllum h yperbolicum Crickmay Among the first rugose coral Assemblage, Acanthophyllum cf. guitangense and Tryplasma el. guangxiensis have been recorded from the Lower Devonian (Emsian) Guitang Formation of Guangxi, Calceola intermediata intermediata and Calceola sandalina nanningensis have hitherto been known from the Lower Devonian (lower Em- sian) Yukiang Formation of Guangxi and the Pochiao Formation of SE Yunnan respectively. Australop
分 类 号:Q915[天文地球—古生物学与地层学]
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