Literature DB >> 17745963

Foraminifera and chlorophyll maximum: vertical distribution, seasonal succession, and paleoceanographic significance.

R G Fairbanks, P H Wiebe.   

Abstract

Many planktonic foraminiferal species deposit their shells at the chlorophyll maximum zone, and it is the temperature range here that is relevant to oceanographic models which use ratios of oxygen-18 to oxygen-16 in fossil foraminifera and foraminiferal fossil assemblages to ascertain past climates. During periods of stratification of the upper water column, the temperature at the chlorophyll maximum may differ from the sea surface temperature by 10 degrees C in the western North Atlantic.

Entities:  

Year:  1980        PMID： 17745963     DOI： 10.1126/science.209.4464.1524

Source DB:  PubMed          Journal:  Science        ISSN： 0036-8075            Impact factor:   47.728


  3 in total

1.  Deep Chlorophyll Maxima in the Global Ocean: Occurrences, Drivers and Characteristics.

Authors:  M Cornec; H Claustre; A Mignot; L Guidi; L Lacour; A Poteau; F D'Ortenzio; B Gentili; C Schmechtig
Journal:  Global Biogeochem Cycles       Date:  2021-04-08       Impact factor: 6.500

2.  Isotopic disequilibrium in Globigerina bulloides and carbon isotope response to productivity increase in Southern Ocean.

Authors:  K Prasanna; Prosenjit Ghosh; S K Bhattacharya; K Mohan; N Anilkumar
Journal:  Sci Rep       Date:  2016-02-23       Impact factor: 4.379

3.  Towards a morphological metric of assemblage dynamics in the fossil record: a test case using planktonic foraminifera.

Authors:  Allison Y Hsiang; Leanne E Elder; Pincelli M Hull
Journal:  Philos Trans R Soc Lond B Biol Sci       Date:  2016-04-05       Impact factor: 6.237
  3 in total

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