Biochronostratigraphy of the western equatorial Atlantic for the last 1.93 Ma
Datos Bibliográficos
| ID | 14978436 |
|---|---|
| Autores | Fabrício Ferreira (0000-0001-9811-4409), Cleverson G Silva, Allan S Oliveira, Cristiano Mazur Chiessi (0000-0003-3318-8022), Andrea Kern (0000-0002-9343-0696), Paul A Baker (0000-0001-9438-855X), Gary Dwyer, Catherine A Rigsby, Enqing Huang (0000-0002-9290-2719), Jun Tian (0000-0002-4842-7076) |
| Año | 2021 |
| Volumen | 598 |
| Páginas | 24-37 |
| Fecha de publicación | 2021-10-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Quaternary International (JOURNAL) |
| Identificadores de la revista | ISSN: 1040-6182 • E-ISSN: 1873-4553 |
| Editorial | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.quaint.2021.04.042 |
| OpenAlex | W3095764304 |
| Idioma | EN |
| Referencias citadas | 52 |
Benthic zone · Foraminifera · Globigerinoides · Latitude · Plankton · Pleistocene · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Paleontology and Stratigraphy of Fossils · Geology · Oceanography · Paleontology
Correlated Millennial-Scale Changes in Surface Hydrography and Terrigenous Sediment Yield Inferred from Last-Glacial Marine Deposits off Northeastern Brazil
Late Pleistocene Paleoclimatology, Foraminiferal Biostratigraphy and Tephrochronology, Western Gulf of Mexico
Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma
An optimized scheme of lettered marine isotope substages for the last 1.0 million years, and the climatostratigraphic nature of isotope stages and substages
An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677
Flexible paleoclimate age-depth models using an autoregressive gamma process
Changes in the water column structure and paleoproductivity in the western South Atlantic Ocean since the middle Pleistocene
IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP
| Velocidad de citación | historical |
|---|---|
| Altamente citado | No |