SFB754 Long gravity cores and piston cores

Fuente: PANGAEA
Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Salvatteci, Renato, Mehrtens, Hela
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2021
Schlagworte:
Climate - Biogeochemistry Interactions in the Tropical Ocean; Cruise/expedition; Date/Time of event; ELEVATION; Event label; GC; GC1; GC10; GC11; GC12; GC13; GC14; GC15; GC16; GC17; GC18; GC19; GC2; GC20; GC21; GC22; GC23; GC3; GC-3; GC4; GC5; GC6; GC7; GC8; GC-8; GC9; Gear; Gravity corer; Latitude of event; Longitude of event; M135; M135_219-3; M135_249-3; M135_249-4; M135_250-3; M135_252-3; M135_254-3; M77/1; M77/1_413; M77/1_414; M77/1_415; M77/1_416; M77/1_417; M77/1_418; M77/1_422; M77/1_493; M77/1_494; M77/1_495; M77/1_496; M77/1_497; M77/1_502; M77/1_503; M77/1_504; M77/1_505; M77/1_506; M77/1_507; M77/1_508; M77/1_509; M77/1_510; M77/1_511; M77/1_512; M77/2; M77/2_002-6; M77/2_003-2; M77/2_005-1; M77/2_005-3; M77/2_022-1; M77/2_024-5; M77/2_026-1; M77/2_028-3; M77/2_029-1; M77/2_029-3; M77/2_045-4; M77/2_047-2; M77/2_050-4; M77/2_052-2; M77/2_053-2; M77/2_054-1; M77/2_056-3; M77/2_056-5; M77/2_059-1; M77/2_060-3; M77/2_062-1; M77/2_064-3; M77/2_065-1; M77/2_067-4; M77/2_069-1; M77/2_072-3; M77/2_075-1; M77/2_076-4; M77/2_635-7; M77/2_636-1; M77/2_639-1; M77/2_647-1; M77/2_668; M77/2_677; M77/2_679; M77/2_686; M77/2_688; M77/2_690; M77/2_718; M77/2_722; M77/2_730; M77/2_733; M77/2_737; M77/2_739; M77/2_746; M77/2_748; M77/2_752; M77/2_758; M77/2_761; M77/2_768; M77/2_770; M77/2_778; M77/2_780; M77/2_791; M77/2_795; M77/2_802; M92; M92_0254-1; M92_0255-1; M92_0263-1; M92_0265-1; M92_0268-1; Meteor (1986); PC; Piston corer; Recovery; Reference/source; Sample code/label; SFB754; SFB754/POSTRE-II
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_version_ 1867171872243712000
author Salvatteci, Renato
Mehrtens, Hela
author_facet Salvatteci, Renato
Mehrtens, Hela
collection Datos científicos de ciencias marinas y ambientales
contents One of the objectives of the SFB 754 was the reconstruction of the factors controlling the intensity and the spatial extent of the OMZ in the Eastern Tropical Pacific, specifically off Peru, since the Last Glacial Maximum (21000 years ago). For the purpose of these paleoceanographic studies, long gravity cores were recovered during four scientific expeditions (M77/1, M77/2, M92, and M135). During the cruises M77/1 and M77/2 in 2008, 51 sediment cores were retrieved below and in the centre of the OMZ, from ~17° S to the equator (Pfannkuche et al., 2011; see Figure 4). Most of the records collected in the core of the OMZ (i.e. ~200 to ~500 m depth), from ~8 to 15° S, show sedimentary discontinuities during the Holocene (last 11700 years), which preclude high resolution paleoceanographic reconstructions in this area (Erdem et al., 2016; Salvatteci et al., 2014, 2016). Based on the information collected during M77/1 and M77/2 and also on the scientific literature, cruise M135 aimed specifically at finding the most complete Holocene sequence in the Eastern Tropical South Pacific. For this purpose, a detailed paleoceanographic survey took place at ~17° S, an area that is less affected by processes that can produce sediment discontinuities.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_927043
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle SFB754 Long gravity cores and piston cores
Salvatteci, Renato
Mehrtens, Hela
Climate - Biogeochemistry Interactions in the Tropical Ocean; Cruise/expedition; Date/Time of event; ELEVATION; Event label; GC; GC1; GC10; GC11; GC12; GC13; GC14; GC15; GC16; GC17; GC18; GC19; GC2; GC20; GC21; GC22; GC23; GC3; GC-3; GC4; GC5; GC6; GC7; GC8; GC-8; GC9; Gear; Gravity corer; Latitude of event; Longitude of event; M135; M135_219-3; M135_249-3; M135_249-4; M135_250-3; M135_252-3; M135_254-3; M77/1; M77/1_413; M77/1_414; M77/1_415; M77/1_416; M77/1_417; M77/1_418; M77/1_422; M77/1_493; M77/1_494; M77/1_495; M77/1_496; M77/1_497; M77/1_502; M77/1_503; M77/1_504; M77/1_505; M77/1_506; M77/1_507; M77/1_508; M77/1_509; M77/1_510; M77/1_511; M77/1_512; M77/2; M77/2_002-6; M77/2_003-2; M77/2_005-1; M77/2_005-3; M77/2_022-1; M77/2_024-5; M77/2_026-1; M77/2_028-3; M77/2_029-1; M77/2_029-3; M77/2_045-4; M77/2_047-2; M77/2_050-4; M77/2_052-2; M77/2_053-2; M77/2_054-1; M77/2_056-3; M77/2_056-5; M77/2_059-1; M77/2_060-3; M77/2_062-1; M77/2_064-3; M77/2_065-1; M77/2_067-4; M77/2_069-1; M77/2_072-3; M77/2_075-1; M77/2_076-4; M77/2_635-7; M77/2_636-1; M77/2_639-1; M77/2_647-1; M77/2_668; M77/2_677; M77/2_679; M77/2_686; M77/2_688; M77/2_690; M77/2_718; M77/2_722; M77/2_730; M77/2_733; M77/2_737; M77/2_739; M77/2_746; M77/2_748; M77/2_752; M77/2_758; M77/2_761; M77/2_768; M77/2_770; M77/2_778; M77/2_780; M77/2_791; M77/2_795; M77/2_802; M92; M92_0254-1; M92_0255-1; M92_0263-1; M92_0265-1; M92_0268-1; Meteor (1986); PC; Piston corer; Recovery; Reference/source; Sample code/label; SFB754; SFB754/POSTRE-II
One of the objectives of the SFB 754 was the reconstruction of the factors controlling the intensity and the spatial extent of the OMZ in the Eastern Tropical Pacific, specifically off Peru, since the Last Glacial Maximum (21000 years ago). For the purpose of these paleoceanographic studies, long gravity cores were recovered during four scientific expeditions (M77/1, M77/2, M92, and M135). During the cruises M77/1 and M77/2 in 2008, 51 sediment cores were retrieved below and in the centre of the OMZ, from ~17° S to the equator (Pfannkuche et al., 2011; see Figure 4). Most of the records collected in the core of the OMZ (i.e. ~200 to ~500 m depth), from ~8 to 15° S, show sedimentary discontinuities during the Holocene (last 11700 years), which preclude high resolution paleoceanographic reconstructions in this area (Erdem et al., 2016; Salvatteci et al., 2014, 2016). Based on the information collected during M77/1 and M77/2 and also on the scientific literature, cruise M135 aimed specifically at finding the most complete Holocene sequence in the Eastern Tropical South Pacific. For this purpose, a detailed paleoceanographic survey took place at ~17° S, an area that is less affected by processes that can produce sediment discontinuities.
title SFB754 Long gravity cores and piston cores
topic Climate - Biogeochemistry Interactions in the Tropical Ocean; Cruise/expedition; Date/Time of event; ELEVATION; Event label; GC; GC1; GC10; GC11; GC12; GC13; GC14; GC15; GC16; GC17; GC18; GC19; GC2; GC20; GC21; GC22; GC23; GC3; GC-3; GC4; GC5; GC6; GC7; GC8; GC-8; GC9; Gear; Gravity corer; Latitude of event; Longitude of event; M135; M135_219-3; M135_249-3; M135_249-4; M135_250-3; M135_252-3; M135_254-3; M77/1; M77/1_413; M77/1_414; M77/1_415; M77/1_416; M77/1_417; M77/1_418; M77/1_422; M77/1_493; M77/1_494; M77/1_495; M77/1_496; M77/1_497; M77/1_502; M77/1_503; M77/1_504; M77/1_505; M77/1_506; M77/1_507; M77/1_508; M77/1_509; M77/1_510; M77/1_511; M77/1_512; M77/2; M77/2_002-6; M77/2_003-2; M77/2_005-1; M77/2_005-3; M77/2_022-1; M77/2_024-5; M77/2_026-1; M77/2_028-3; M77/2_029-1; M77/2_029-3; M77/2_045-4; M77/2_047-2; M77/2_050-4; M77/2_052-2; M77/2_053-2; M77/2_054-1; M77/2_056-3; M77/2_056-5; M77/2_059-1; M77/2_060-3; M77/2_062-1; M77/2_064-3; M77/2_065-1; M77/2_067-4; M77/2_069-1; M77/2_072-3; M77/2_075-1; M77/2_076-4; M77/2_635-7; M77/2_636-1; M77/2_639-1; M77/2_647-1; M77/2_668; M77/2_677; M77/2_679; M77/2_686; M77/2_688; M77/2_690; M77/2_718; M77/2_722; M77/2_730; M77/2_733; M77/2_737; M77/2_739; M77/2_746; M77/2_748; M77/2_752; M77/2_758; M77/2_761; M77/2_768; M77/2_770; M77/2_778; M77/2_780; M77/2_791; M77/2_795; M77/2_802; M92; M92_0254-1; M92_0255-1; M92_0263-1; M92_0265-1; M92_0268-1; Meteor (1986); PC; Piston corer; Recovery; Reference/source; Sample code/label; SFB754; SFB754/POSTRE-II
url https://doi.org/10.1594/PANGAEA.927043