Globorotalia truncatulinoides' Growth and chemistry as probes of the past thermocline: 1. Shell size
- 1 February 1990
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 5 (1) , 55-75
- https://doi.org/10.1029/pa005i001p00055
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- Seasonally abundant planktonic foraminifera of the Sargasso Sea; succession, deep-water fluxes, isotopic compositions, and paleoceanographic implicationsJournal of Foraminiferal Research, 1989
- Field and laboratory studies on the ontogeny and ecology of some globorotaliid species from the Sargasso Sea off BermudaJournal of Foraminiferal Research, 1985
- Taxonomic and ecological significance of embryonic and juvenile planktonic foraminiferaJournal of Foraminiferal Research, 1985
- Paleo-oceanographic utility of oxygen isotopic measurements on planktic foraminifera: Indian Ocean core-top evidencePalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Seasonal changes in species composition, numbers, mass, size, and isotopic composition of planktonic foraminifera settling into the deep sargasso seaPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Seasonal stable isotopic variations in living planktonic foraminifera from bermuda plankton towsPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Non-equilibrium isotopic compositions of shells of planktonic foraminifera in the Mediterranean seaPalaeogeography, Palaeoclimatology, Palaeoecology, 1976
- Insensitivity of subtropical mode water characteristics to meteorological fluctuationsDeep Sea Research and Oceanographic Abstracts, 1972
- Variations in coiling ratios of Holocene planktonic foraminiferaDeep Sea Research and Oceanographic Abstracts, 1971
- Ecology of Recent Planktonic Foraminifera: Part 2: Bathymetric and Seasonal Distributions in the Sargasso Sea off BermudaMicropaleontology, 1960