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Paleoecology of Sponge-?Hydroid Associations in Silurian Microbial Reefs

机译:志留纪微生物礁海绵体-类脂体结合的古生态学

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摘要

Microbial boundstones from Alaska and Russia yield new insights into the paleoecology of Silurian biotas that inhabited stromatolite reefs. These high-energy reefs were built along the Uralian Seaway in the Late Silurian by a diverse suite of microorganisms in association with accessory metazoans, predominantly sphinctozoan sponges. Within the stromatolite framework, three species of small, solitary, sphinctozoans (aphrosalpingids) encrusted a variety of hard substrates, mostly skeletal remains but also microbial laminae and cavity surfaces. Fossils encrusted by the sponges include the problematic hydroid Fistulella, possible stromatoporoids (recrystallized), crinoids, the possible cyanobacterium Ludlovia, corals, and unidentifiable shelly debris. In addition to the ubiquitous microbial laminae, the sponges, Fistulella, and ?stromatoporoids were less commonly encrusted by Ludlovia, Renalcis, or crinoids.
机译:来自阿拉斯加和俄罗斯的微生物胶结石对居住在叠层石 礁中的志留系生物群的古生态学产生了新的见解。这些高能礁是由志留纪晚期的乌拉尔 海道沿岸,由多种微生物 与附属后生动物(主要是括约动物 )结合而成的。海绵。在叠层石框架内,三种 小型,单生的括约动物(aphrosalpingids)包裹着各种硬底物,主要是骨骼残留物,还包括 微生物薄片和型腔表面。由 海绵包裹的化石包括有问题的水硬瘘,可能的 间质多孔(重结晶),海百合,可能的蓝细菌,Ludlovia,珊瑚和无法识别的贝壳碎片。除了 ,普遍存在的微生物层中,海绵,瘘孔菌, 和?stromatoporoids很少被Ludlovia, Rinalcis或海百合包裹。 sup>

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  • 来源
    《PALAIOS》 |2003年第3期|225-235|共11页
  • 作者单位

    Department of Geology, Colgate University, Hamilton, NY 13346, csoja@mail.colgate.edu;

    Department of Geology, Colgate University, Hamilton, NY 13346, csoja@mail.colgate.edu;

    Department of Geology, Colgate University, Hamilton, NY 13346, csoja@mail.colgate.edu;

    Department of Geology, Colgate University, Hamilton, NY 13346, csoja@mail.colgate.edu;

    Department of Geology, Colgate University, Hamilton, NY 13346, csoja@mail.colgate.edu;

    Institute of Geology, Komi Science Centre, 54 Pervomayskaya Street, Syktyvkar 167982, Russia;

    Department of Geology, Smith College, Northampton, MA 01063;

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