N J SHACKLETON
Biographic Data
| ID | 5218997 |
|---|---|
| NAME | N J SHACKLETON |
| GIVEN NAMES | N J |
| FAMILY NAME | SHACKLETON |
| SIGNATURE | SHACKLETON N J |
| AFFILIATIONS | University of Cambridge |
| VERIFIED | No |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1976 |
| LATEST PUBLICATION YEAR | 1999 |
| H-INDEX | 0 |
Dansgaard‐Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures
Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C 37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ∼200 years allowing the study of millennial‐scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling eve…
The deep-sea sediment record and the Pliocene-Pleistocene boundary
Towards a Quaternary Time Scale
Nine first-appearance datums (FADs), twenty-three last-appearance datums (LADs), and three other micropaleontological datums are related to the magnetic-reversal, oxygen-isotope, and calcite-dissolution/coarse-fraction time scales to provide a preliminary basis for subdivision of the Quaternary in deep-sea sediments. The magnetic-reversal, oxygen-isotope, and calcite-dissolution/coarse-fraction scales have been correlated by determination on the …
Variations in the Earth's Orbit: Pacemaker of the Ice Ages
1) Three indices of global climate have been monitored in the record of the past 450,000 years in Southern Hemisphere ocean-floor sediments. 2) Over the frequency range 10 –4 to 10 –5 cycle per year, climatic variance of these records is concentrated in three discrete spectral peaks at periods of 23,000, 42,000, and approximately 100,000 years. These peaks correspond to the dominant periods of the earth's solar orbit, and contain respectively abo…
No prominent works on this page.
Variations in the Earth's Orbit: Pacemaker of the Ice Ages
1) Three indices of global climate have been monitored in the record of the past 450,000 years in Southern Hemisphere ocean-floor sediments. 2) Over the frequency range 10 –4 to 10 –5 cycle per year, climatic variance of these records is concentrated in three discrete spectral peaks at periods of 23,000, 42,000, and approximately 100,000 years. These peaks correspond to the dominant periods of the earth's solar orbit, and contain respectively abo…
Towards a Quaternary Time Scale
Nine first-appearance datums (FADs), twenty-three last-appearance datums (LADs), and three other micropaleontological datums are related to the magnetic-reversal, oxygen-isotope, and calcite-dissolution/coarse-fraction time scales to provide a preliminary basis for subdivision of the Quaternary in deep-sea sediments. The magnetic-reversal, oxygen-isotope, and calcite-dissolution/coarse-fraction scales have been correlated by determination on the …
The deep-sea sediment record and the Pliocene-Pleistocene boundary
Dansgaard‐Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures
Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C 37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ∼200 years allowing the study of millennial‐scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling eve…
Geology and Paleoclimatology Research (4 works) · Geology (3 works) · Paleontology (3 works) · Climatology (2 works) · Glacial period (2 works) · Isotope Analysis in Ecology (2 works) · Oceanography (2 works) · Paleontology and Stratigraphy of Fossils (2 works) · Quaternary (2 works) · Astronomy (1 work)