CHITINOZOAN BIOFACIES OF LATE EARLY LLANDOVERY (CORONOGRAPTUS CYPHUS) AGE IN THE EAST BALTIC

V. Nestor
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引用次数: 10

Abstract

. 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.
东波罗的海陆生动物(coronograptus cyphus)晚期早期几丁虫生物相
. 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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