Published February 24, 2012 | Version v1
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Fig. 4 in Origin and significance of Late Cretaceous bioevents: Examples from the Cenomanian

Description

Fig. 4. Sketch (strongly vertically exaggerated) explaining the formation of early transgressive bioevents of the lag subtype with resultant stratigraphic section in Cenomanian epicontinental shelf settings of NW Europe. Abbreviations: FWWB, fair−weather wave−base; HST, highstand systems tract; SWB, storm wave−base; TST, transgressive systems tract. For key of symbols see Fig. 9.

Notes

Published as part of Wilmsen, Markus, 2012, Origin and significance of Late Cretaceous bioevents: Examples from the Cenomanian, pp. 759-771 in Acta Palaeontologica Polonica 57 (4) on page 762, DOI: 10.4202/app.2011.0044, http://zenodo.org/record/13279227

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Journal article: 10.4202/app.2011.0044 (DOI)
Journal article: urn:lsid:plazi.org:pub:B778FFFFBD00FFF89F47FFD3FFCAFFF6 (LSID)
Journal article: https://zenodo.org/record/13279227 (URL)