Abstract
Macrofossils in deep wells are usually very well preserved. The Middle Jurassic macrofloras in the northernmostNorth Sea are closely related to those in the Cleveland Basin, England. The Late Jurassic macrofloras resemble those from the east coast of Scotland. The macrofaunas in the Late Jurassic formations of the Northern North Sea are related with those in the Kimmeridge Clay Formation of the Southern North Sea. However, differences in palaeoenvironments are recognised as examplified by mass occurrences of squids and lingulid brachiopods, which are characteristic elements in the Draupne Formation.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
