西爱沙尼亚岩心中Margachitina margaritana生物带和Llandovery-Wenlock边界的几丁质动物

V. Nestor
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引用次数: 10

摘要

. 本文描述了Viki、Ohesaare、Kaugatuma和Ruhnu钻孔岩心剖面中Llandovery上部和Wenlock下部几丁动物类群的演变,并与英国什罗普郡Hughley Brook基底Wenlock的全球层型剖面进行了对比。爱沙尼亚剖面中llanddovery (cid:150)Wenlock边界最重要的生物标志物是Ramochitina nestorae, Conochitina acuminata, C。cf. flamma和Angochitina longicollis。在西爱沙尼亚岩心中,这个边界对应于Margachitina margaritana生物带中部或上部的一个水平。在Viki和Ohesaare岩心中,它与Adavere和Jaani区域阶段的公认边界之上的膨润土层一致,并与murchisoni笔石生物带中部的一个水平相关。报道了Belonechitina oeselensis、anyrochitina mullinsi和Eisenackitina inanulifera 3个新种。
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Chitinozoans of the Margachitina margaritana Biozone and the Llandovery–Wenlock boundary in West Estonian drill cores
. The succession of chitinozoan taxa in the uppermost Llandovery and lowermost Wenlock of the Viki, Ohesaare, Kaugatuma, and Ruhnu drill core sections is described and correlated with the global stratotype section of the basal Wenlock in Hughley Brook, Shropshire, England. The most important biomarkers for the identification of the Llandovery(cid:150)Wenlock boundary in Estonian sections are the disappearance levels of Ramochitina nestorae , Conochitina acuminata , C . cf. flamma , and Angochitina longicollis . In the West Estonian cores this boundary corresponds to a level in the middle or upper part of the Margachitina margaritana Biozone. In the Viki and Ohesaare cores it coincides with the bentonite layers above the accepted boundary between the Adavere and Jaani regional stages and correlates with a level in the middle of the murchisoni graptolite Biozone. Three new species, Belonechitina oeselensis , Ancyrochitina mullinsi , and Eisenackitina inanulifera , are described.
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Hydrogeological model of Estonia and its applications CHITINOZOAN BIOFACIES OF LATE EARLY LLANDOVERY (CORONOGRAPTUS CYPHUS) AGE IN THE EAST BALTIC WENLOCKIAN AND LUDLOVIAN SEDIMENTARY AND BIOTIC EVENTS IN THE MIDWESTERN CRATONIC AREA, U.S.A. PRELIMINARY RESULTS AND INTERPRETATIONS OF MINERAL MAGNETIC ANALYSES OF A HOLOCENE SEDIMENT SUCCESSION FROM LAKE MAARDU NEAR TALLINN, ESTONIA РАДОНОВЫЙ ФАКТОР РАДИАЦИОННОГО ФОНА В НАСЕЛЕННЫХ ПУНКТАХ СЕВЕРНОЙ ЭСТОНИИ (ЭКОГЕОЛОГИЧЕСКИЙ АСПЕКТ)
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