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{{H-TestTemplate4 |Author(s)=M.B. Hart, W. Hudson, C.W. Smart, J. Tyszka |Publication Year=2012 |Source (e.g. journal, book)=Journal of Micropalaeontology 31, 97-109. |Age=Jurassic |Subject(s)=Taxonomy, (Palae)oceanography |Annotation=‘Globigerina Ooze’, Foraminiferal Ooze or Carbonate Ooze as it is now known, is a widespread and highly characteristic sediment of the modern ocean system. Comparable sediments are much less common in the geological record although, as we describe here, a number of Middle Jurassic carbonate sediments with distinctive assemblages from Central Europe fulfil many of the criteria. One important component of these assemblages in the Middle Jurassic is ''Globigerina bathoniana'' Pazdrowa, 1969, first described from the Bathonian sediments near Ogrodzieniec (Poland). .... }} A test page.
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