Thermocline-level connectivity between the tropical equatorial Pacific and tropical northeast Pacific during deglaciation
Bibliographic Data
| ID | 14972391 |
|---|---|
| Authors | Alberto Sánchez (0000-0002-1294-3044), José Carriquiry |
| Year | 2024 |
| Volume | 705 |
| Pages | 86-93 |
| Publication date | 2024-09-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary International (JOURNAL) |
| Journal identifiers | ISSN: 1040-6182 • E-ISSN: 1873-4553 |
| Publisher | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.quaint.2024.03.010 |
| OpenAlex | W4394015379 |
| Language | EN |
| References cited | 66 |
Benthic zone · Circumpolar deep water · Deglaciation · Foraminifera · Holocene · Last Glacial Maximum · North Atlantic Deep Water · Oxygen minimum zone · Sea surface temperature · Stable isotope ratio · Thermocline · Thermohaline circulation · Tropical Atlantic · Upwelling · Water mass · Younger Dryas · δ18O · Geology and Paleoclimatology Research · Marine Biology and Ecology Research · Methane Hydrates and Related Phenomena · Geology · Oceanography
Revised Carbonate-Water Isotopic Temperature Scale
Hydrothermal carbon release to the ocean and atmosphere from the eastern equatorial Pacific during the last glacial termination
Carbon isotope minima in the South Atlantic during the last deglaciation
The paleoclimatic response of the Southern Californian Margin to the rapid climate change of the last 60ka
| Highly cited | No |
|---|