Results 161 to 170 of about 7,479 (224)

Multidisciplinary evidence for synchroneity between Ontong Java Nui volcanism and early Aptian oceanic anoxic event 1a. [PDF]

open access: yesSci Adv
Matsumoto H   +8 more
europepmc   +1 more source

Zonally asymmetric changes in the Antarctic Circumpolar Current strength over the past million years. [PDF]

open access: yesNat Geosci
Wu S   +8 more
europepmc   +1 more source

Repeated major inland retreat of Thwaites and Pine Island glaciers (West Antarctica) during the Pliocene. [PDF]

open access: yesProc Natl Acad Sci U S A
Horikawa K   +13 more
europepmc   +1 more source
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C. -Les Nannofossiles calcaires/ Calcareous nannofossils

Géologie Méditerranéenne, 1979
Muller C., Templeton R.S.M., Desprat R. C. -Les Nannofossiles calcaires/ Calcareous nannofossils. In: Géologie Méditerranéenne. Tome 6, numéro 1, 1979. La mer pélagienne. Etude sédimentologique et écologique du Plateau tunisien et du Golfe de Gabès. pp. 210-220.
Müller, Carla   +2 more
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Calcareous nannofossils

1996
Abstract This chapter deals with calcareous nannofossils or coccoliths. These range in size from 1-100 µ,. Preparation of samples for calcareous nannofossil study generally consists of pulverising the containing sediment in distilled water using a pestle and mortar, strewing some of the suspended mixture onto a slide using a pipette and ...
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Calcareous Nannofossil Biostratigraphy

1998
List of Contributors. Preface. Technical note and abbreviations. 1. Introduction p P.R. Bown, J.R. Young. 2. Techniques P.R. Bown, J.R. Young. 3. Triassic P.R. Bown. 4. Jurassic P.R. Bown, M.K.E. Cooper. 5. Lower Cretaceous P.R. Bown, D.C. Rutledge, J.A. Crux, L.T. Gallagher. 6. Upper Cretaceous J.A. Burnett. 7. Palaeogene O. Varol. 8.
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Nannofossils and biostratigraphy: An overview

Earth-Science Reviews, 1977
Abstract Intensive biostratigraphic studies of calcareous nannofossils have been carried out for only about a decade, even though nannofossils have been known for over a century. Although coccoliths have been reported from various Paleozoic deposits, datable assemblages are known only from Liassic (early Jurassic) and younger strata.
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