Alkenone unsaturation index and alkenones in ODP Hole 161-977A

• Main Author: Martrat, Belén
• Format: Dataset
• Language: English
• Published: PANGAEA 2007
• Subjects: 161-977A; AGE; Alboran Sea; Alkenone; C37:2Me+C37:3Me; unsaturation index UK'37; Calculated from UK'37 (Müller et al; 1998); DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg161; Ocean Drilling Program; ODP; Sample code/label; Sea surface temperature; annual mean; Bjørnøya; Ice Sheet
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.819829; https://doi.org/10.1594/PANGAEA.819829

A number of essential elements closely related to each other are involved in the Earth's climatic system. The temporal and spatial distribution of insolation determines wind patterns and the ocean's thermohaline pump. In turn, these last two are directly linked to the extension and retreat of marine and continental ice and to the chemistry of the atmosphere and the ocean. The variability of these elements may trigger, amplify, sustain or globalize rapid climatic changes. Paleoclimatic oscillations have been identified in this thesis by using fossil organic compounds synthesized by marine and terrestrial flora. High sedimentation rate deposits at the Barents and the Iberian peninsula continental margins were chosen in order to estimate the climatic changes on centennial time resolution. At the Barents margin, the sediment recovered was up to 15,000 years old (unit ''a'', from latin ''annos'') (M23258; west of the Bjørnøya island). At the Iberian margin, the sediment cores studied covered a wide range of time spans: up to 115,000 a (MD99-2343; north of the Minorca island), up to 250,000 a (ODP-977A; Alboran basin) and up to 420,000 a (MD01-2442, MD01-2443, MD01-2444, MD01-2445; close to the Tagus abyssal plain). At the northern site, inputs containing marine, continental and ancient reworked organic matter provided a detailed reconstruction of climate history at the time of the final retreat of the Barents ice sheet. At the western Barents continental slope, warm climatic conditions were observed during the early Holocene (~from 8,650 a to 5,240 a ago); in contrast, an apparent long-term cooling trend occurred in the late Holocene (~from 5,240 a to 760 a ago), in consistence with other paleoarchives from northern and southern European latitudes. The Iberian margin sites, which were never covered with large ice sheets, preserved exceptionally complete sequences of rapid events during ice ages hitherto not studied in such great detail: during the last glacial (~from 70,900 a to 11,800 a ago), the second glacial ...