Skip Nav Destination
Article navigation
Other|
April 01, 1992
The relationship between sediment fabric and planktonic microfossil taphonomy; how do plankton skeletons become pelagic ooze?
Amanda Palmer-Julson;
Amanda Palmer-Julson
Ocean Drill. Program, College Station, TX, United States
Search for other works by this author on:
PALAIOS (1992) 7 (2): 167–177.
Article history
first online:
03 Mar 2017
Citation
Amanda Palmer-Julson, F. R. Rack; The relationship between sediment fabric and planktonic microfossil taphonomy; how do plankton skeletons become pelagic ooze?. PALAIOS 1992;; 7 (2): 167–177. doi: https://doi.org/10.2307/3514927
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Email alerts
Index Terms/Descriptors
Latitude & Longitude
Citing articles via
Related Articles
Barbados Ridge; inner trench slope sedimentation
Journal of Sedimentary Research
Essai de caracterisation de quelques regimes sedimentaires ayant prevalu sur la marge nord du golfe de Gascogne depuis le debut du Cenozoique
Bulletin de la Société Géologique de France
Related Book Content
Taphonomy and sedimentology of Arikaree (lower Miocene) fluvial, eolian, and lacustrine paleoenvironments, Nebraska and Wyoming; A paleobiota entombed in fine-grained volcaniclastic rocks
Volcanism and Fossil Biotas
Gamma-ray attenuation bulk density as an indicator of diatom valve abundance and fragmentation in Pleistocene biosiliceous sediments of the Bering Sea
Understanding the Monterey Formation and Similar Biosiliceous Units across Space and Time
Stratigraphic development of southwestern Panama as determined from integration of marine seismic data and onshore geology
Geologic and Tectonic Development of the Caribbean Plate Boundary in Southern Central America
Unconventional Gas-Oil Shale Microfabric Features Relating to Porosity, Storage, and Migration of Hydrocarbons
Imaging Unconventional Reservoir Pore Systems