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REVISION OF THE SILURIAN BRACHIOPOD PENTAMERUS SAMOJEDICUS KEYSERLING, 1846 FROM THE TIMAN RIDGE, RUSSIA 俄国提曼岭志留纪腕足动物pentamerus samojedicus keyserling的修正
Pub Date : 1900-01-01 DOI: 10.3176/geol.2000.2.06
T. L. Modzalevskaya, M. Rubel
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引用次数: 2
MAARDLATE HÕLVAMISE PÕHIPROBLEEMIDEST EESTIS
Pub Date : 1900-01-01 DOI: 10.3176/geol.1991.1.05
A. Teedumäe
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引用次数: 0
DIMITRI KALJO 70; p. 262 迪米特里·卡约70;262页。
Pub Date : 1900-01-01 DOI: 10.3176/geol.1998.4.04
A. Raukas, R. Vaikmäe
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引用次数: 0
Professor Lars-Konig KÖNIGSSON
Pub Date : 1900-01-01 DOI: 10.3176/geol.1998.1.04
A. Raukas, L. Saarse, R. Vaikmäe
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引用次数: 0
CHITINOZOAN BIOFACIES OF LATE EARLY LLANDOVERY (CORONOGRAPTUS CYPHUS) AGE IN THE EAST BALTIC 东波罗的海陆生动物(coronograptus cyphus)晚期早期几丁虫生物相
Pub Date : 1900-01-01 DOI: 10.3176/geol.1998.4.01
V. Nestor
. Four lateral chitinozoan biofacies, mainly defined by the distribution of Cyathochitina species, are recognized from the uppermost lower Llandovery strata (Coronograptus cyphus age) in 18 eastern Baltic sections. Cyathochitina kuckersiana (Eisenack, 1934) seems to have preferred shallow-water near-shore conditions and С. сайх (Eisenack, 1931) deeper parts of the shelf, whereas C. campanulaeformis (Eisenack, 1931) is more widespread. Representatives of the genus Cyathochitina appear to be absent in most of the near-shore environment. However, these chitinozoan biofacies are probably of only regional significance and occur where calcareous muds (which formed calcilutites) were deposited.
. 在波罗的海东部18个剖面的Llandovery地层(Coronograptus cyphus时代)中,发现了4种侧向几丁虫生物相,主要以壳虫种的分布为界。Cyathochitina kuckersiana (Eisenack, 1934)似乎更喜欢浅水近岸环境和С。сайх (Eisenack, 1931)较深的陆架部分,而C. campanulaeformis (Eisenack, 1931)更为广泛。在大多数近岸环境中似乎没有花壳属的代表。然而,这些几丁质动物生物相可能仅具有区域意义,并发生在沉积钙质泥(形成钙质岩)的地方。
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引用次数: 10
MINERALOGY AND MICROPALAEONTOLOGY OF THE KINNEKULLE ALTERED VOLCANIC ASH BED (ORDOVICIAN) AT PÄÄSKÜLA, NORTH ESTONIA 爱沙尼亚北部pÄÄskÜla kinnekulle蚀变火山灰床(奥陶系)的矿物学和微古生物学
Pub Date : 1900-01-01 DOI: 10.3176/geol.1997.3.01
O. Hints, T. Kallaste, T. Kiipli
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引用次数: 7
SOOD VEESÄILITUSALADEKS; pp. 197–198
Pub Date : 1900-01-01 DOI: 10.3176/geol.1995.3.06
E. Andresmaa, H. Kink
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引用次数: 0
EVENTS IN THE CONODONT HISTORY DURING THE SILURIAN IN ESTONIA 爱沙尼亚志留纪牙形石历史上的事件
Pub Date : 1900-01-01 DOI: 10.3176/geol.1993.2.03
P. Männik, V. Viira
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引用次数: 2
A NEW SPECIES MEGALOMOIDEA WALLISERI (BIVALVIA) FROM THE SILURIAN OF ESTONIA 文章标题爱沙尼亚志留纪双壳科大壳科walliseri一新种
Pub Date : 1900-01-01 DOI: 10.3176/geol.1993.3.04
M. Isakar, I. Sinicyna
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引用次数: 1
A NEW UPPER SILURIAN CONODONT SPECIES FROM ESTONIA 爱沙尼亚上志留统牙形石一新种
Pub Date : 1900-01-01 DOI: 10.3176/geol.1994.1.03
V. Viira
. A new conodont species Ozarkodina roopaensis sp. n. is described from the Ludlow-age Roopa cliff of the Paadla Formation, corresponding to the uppermost part of the Gorstian Stage. The O. roopaensis conodont Zone represents part of the Ludlow nearshore zonation scale in the East Baltic. The new species of Ozarkodina is related to Ozarkodina confluens, but differs in Pa element having primitive transverse ridges on oral smooth surfaces of denticles. Characteristic is the distribution of white matter.
. 报道了一种新的牙形刺物种Ozarkodina roopaensis sp. n.,来自于Paadla组的Ludlow-age Roopa cliff,对应于Gorstian阶段的最上部。O. roopaensis牙形刺带代表了东波罗的海Ludlow近岸带规模的一部分。该新种与欧扎科地纳属同源,但Pa元素不同,齿齿光滑表面有原始的横脊。特征是白质的分布。
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引用次数: 5
期刊
Proceedings of the Estonian Academy of Sciences. Geology
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