Author:
LOYDELL D. K.,NESTOR V.,MÄNNIK P.
Abstract
AbstractIntegrated graptolite, conodont and chitinozoan biostratigraphical data are presented from the Llandovery and Wenlock of the Kolka-54 core, Latvia. Correlations between graptolite and chitinozoan biozones are consistent with those published from other East Baltic sections and the Welsh Basin. While most correlations between graptolite and conodont biozones agree with those presented in previous studies, there are important exceptions. Significantly, we report here the discovery ofDistomodus staurognathoidesBiozone conodonts in the lowest AeronianDemirastrites triangulatusgraptolite Biozone. The base of theD. staurognathoidesBiozone was previously considered to lie much higher in the Aeronian. Also it is shown thatWalliserodussurvived the late Wenlock Mulde Event, during which it was considered previously to have become extinct.
Publisher
Cambridge University Press (CUP)
Reference42 articles.
1. New chitinozoan taxa from the lower Wenlock (Silurian) of the Welsh Borderlands, England
2. The Wenlock and Ludlow succession in the Howgill Fells (north-west Yorkshire and Westmoreland)
3. Chitinozoan biostratigraphy and lithological characteristics of the Lower and Upper Visby boundary beds in the Ireviken 3 section, Northwest Gotland;Nestor;Proceedings of Estonian Academy of Sciences, Geology,2002
4. Chitinozoan biofacies of late early Llandovery (Coronograptus cyphus) age in the East Baltic;Nestor;Proceedings of Estonian Academy Sciences, Geology,1998
5. Early Silurian chitinozoans of Estonia and North Latvia;Nestor;Academia,1994
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