S Stephen Streeter
Biographic Data
| ID | 11137109 |
|---|---|
| NAME | S Stephen Streeter |
| GIVEN NAMES | S Stephen |
| FAMILY NAME | Streeter |
| SIGNATURE | STREETER S S |
| AFFILIATIONS | Lamont-Doherty Earth Observatory |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1973 |
| LATEST PUBLICATION YEAR | 1984 |
| H-INDEX | 0 |
The Last Interglacial Ocean
The final effort of the CLIMAP project was a study of the last interglaciation, a time of minimum ice volume some 122,000 yr ago coincident with the Substage 5e oxygen isotopic minimum. Based on detailed oxygen isotope analyses and biotic census counts in 52 cores across the world ocean, last interglacial sea-surface temperatures (SST) were compared with those today. There are small SST departures in the mid-latitude North Atlantic (warmer) and t…
Late Pleistocene Paleo-Oceanography of the Norwegian-Greenland Sea
Fluctuations in benthic foraminiferal faunas over the last 130,000 yr in four piston cores from the Norwegian Sea are correlated with the standard worldwide oxygen-isotope stratigraphy. One species, Cibicides wuellerstorfi , dominates in the Holocene section of each core, but alternates downcore with Oridorsalis tener , a species dominant today only in the deepest part of the basin. O. tener is the most abundant species throughout the entire basi…
Bottom Water and Benthonic Foraminifera in the North Atlantic—Glacial-Interglacial Contrasts
Today, below 2500 m, benthonic foraminiferal faunas in the North Atlantic are dominated by a few species. Faunal composition changes slowly with increasing depth and decreasing temperature. Surface sediment and down-core counts of benthonic foraminifera reported by Phleger, Parker, and Peirson (1953) in the reports of the Swedish Deep-Sea Expedition have been supplemented by additional bottom sediment and piston core samples. Present-day benthoni…
No prominent works on this page.
Bottom Water and Benthonic Foraminifera in the North Atlantic—Glacial-Interglacial Contrasts
Today, below 2500 m, benthonic foraminiferal faunas in the North Atlantic are dominated by a few species. Faunal composition changes slowly with increasing depth and decreasing temperature. Surface sediment and down-core counts of benthonic foraminifera reported by Phleger, Parker, and Peirson (1953) in the reports of the Swedish Deep-Sea Expedition have been supplemented by additional bottom sediment and piston core samples. Present-day benthoni…
Late Pleistocene Paleo-Oceanography of the Norwegian-Greenland Sea
Fluctuations in benthic foraminiferal faunas over the last 130,000 yr in four piston cores from the Norwegian Sea are correlated with the standard worldwide oxygen-isotope stratigraphy. One species, Cibicides wuellerstorfi , dominates in the Holocene section of each core, but alternates downcore with Oridorsalis tener , a species dominant today only in the deepest part of the basin. O. tener is the most abundant species throughout the entire basi…
The Last Interglacial Ocean
The final effort of the CLIMAP project was a study of the last interglaciation, a time of minimum ice volume some 122,000 yr ago coincident with the Substage 5e oxygen isotopic minimum. Based on detailed oxygen isotope analyses and biotic census counts in 52 cores across the world ocean, last interglacial sea-surface temperatures (SST) were compared with those today. There are small SST departures in the mid-latitude North Atlantic (warmer) and t…
Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Glacial period (3 works) · Interglacial (3 works) · Isotope Analysis in Ecology (3 works) · Oceanography (3 works) · Paleontology (3 works) · Benthic zone (2 works) · Bottom water (2 works) · Foraminifera (2 works)