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June 01, 1996
Secular increase in nutrient levels through the Phanerozoic; implications for productivity, biomass, and diversity of the marine biosphere Available to Purchase
Ronald E. Martin
Ronald E. Martin
University of Delaware, Department of Geology, Newark, DE, United States
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Ronald E. Martin
University of Delaware, Department of Geology, Newark, DE, United States
Publisher: SEPM Society for Sedimentary Geology
First Online:
03 Mar 2017
Online ISSN: 1938-5323
Print ISSN: 0883-1351
GeoRef, Copyright 2004, American Geological Institute.
PALAIOS (1996) 11 (3): 209–219.
Article history
First Online:
03 Mar 2017
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CitationRonald E. Martin; Secular increase in nutrient levels through the Phanerozoic; implications for productivity, biomass, and diversity of the marine biosphere. PALAIOS 1996;; 11 (3): 209–219. doi: https://doi.org/10.2307/3515230
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Index Terms/Descriptors
- acritarchs
- algae
- alkaline earth metals
- biogenic structures
- biologic evolution
- biomass
- biosphere
- bioturbation
- Bivalvia
- C-13
- carbon
- Cenozoic
- diatoms
- Dinoflagellata
- eutrophication
- extinction
- Foraminifera
- fossil record
- glaciation
- Globigerinacea
- Globigerinidae
- Invertebrata
- isotope ratios
- isotopes
- marine environment
- Mesozoic
- metals
- microfossils
- Mollusca
- Neogene
- nutrients
- ocean circulation
- organic carbon
- organic compounds
- organic materials
- paleo-oceanography
- paleoenvironment
- Paleozoic
- palynomorphs
- Phanerozoic
- plankton
- Plantae
- plate tectonics
- productivity
- Protista
- Radiolaria
- reefs
- regression
- rifting
- Rotaliina
- S-34/S-32
- sea-level changes
- sedimentary structures
- species diversity
- Sr-87/Sr-86
- stable isotopes
- strontium
- sulfur
- Tertiary
- transgression
- weathering
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