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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2011
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.770171 |
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| _version_ | 1867170916144775168 |
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| author | Wienberg, Claudia Frank, Norbert Mertens, Kenneth Neil Stuut, Jan-Berend W Marchant, Margarita Fietzke, Jan Mienis, Furu Hebbeln, Dierk |
| author_facet | Wienberg, Claudia Frank, Norbert Mertens, Kenneth Neil Stuut, Jan-Berend W Marchant, Margarita Fietzke, Jan Mienis, Furu Hebbeln, Dierk |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A set of 40 Uranium-series datings obtained on the reef-forming scleractinian cold-water corals Lophelia pertusa and Madrepora oculata revealed that during the past 400 kyr their occurrence in the Gulf of Cádiz (GoC) was almost exclusively restricted to glacial periods. This result strengthens the outcomes of former studies that coral growth in the temperate NE Atlantic encompassing the French, Iberian and Moroccan margins dominated during glacial periods, whereas in the higher latitudes (Irish and Norwegian margins) extended coral growth prevailed during interglacial periods. Thus it appears that the biogeographical limits for sustained cold-water coral growth along the NE Atlantic margin are strongly related to climate change. By focussing on the last glacial-interglacial cycle, this study shows that palaeo-productivity was increased during the last glacial. This was likely driven by the fertilisation effect of an increased input of aeolian dust and locally intensified upwelling. After the Younger Dryas cold event, the input of aeolian dust and productivity significantly decreased concurrent with an increase in water temperatures in the GoC. This primarily resulted in reduced food availability and caused a widespread demise of the formerly thriving coral ecosystems. Moreover, these climate induced changes most likely caused a latitudinal shift of areas withoptimum coral growth conditions towards the northern NE Atlantic where more suitable environmental conditions established with the onset of the Holocene. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_770171 |
| institution | PANGAEA |
| language | en |
| publishDate | 2011 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Glacial cold-water coral: ages, isotope concentrations and ratios Wienberg, Claudia Frank, Norbert Mertens, Kenneth Neil Stuut, Jan-Berend W Marchant, Margarita Fietzke, Jan Mienis, Furu Hebbeln, Dierk 64PE229; Age, relative; Age, standard deviation; Belgica area off Morocco; Center for Marine Environmental Sciences; Comment of event; Coral; DEPTH, sediment/rock; Event label; Faro/Almazan mud volcano; GAP; GC; GC25; GC27; GC35; GC36; GC44; GeoB9018-1; GeoB9031-1; GeoB9032-1; GeoB9070-1; Gravity corer; Gulf of Cádiz, Atlantic Ocean; HERMIONE; Hesperides mud volcano; Hotspot Ecosystem Research and Mans Impact On European Seas; Latitude of event; Longitude of event; M2004-02_PC; Maria S. Merian; MARUM; Moundforce 2004; MSM01/3; MSM01/3_254; MSM01/3_257; MSM01/3_292; MSM01/3_293; MSM01/3_325; PC; Pelagia; Piston corer; SO175; Sonne; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation; δ234 Uranium; δ234 Uranium, standard deviation A set of 40 Uranium-series datings obtained on the reef-forming scleractinian cold-water corals Lophelia pertusa and Madrepora oculata revealed that during the past 400 kyr their occurrence in the Gulf of Cádiz (GoC) was almost exclusively restricted to glacial periods. This result strengthens the outcomes of former studies that coral growth in the temperate NE Atlantic encompassing the French, Iberian and Moroccan margins dominated during glacial periods, whereas in the higher latitudes (Irish and Norwegian margins) extended coral growth prevailed during interglacial periods. Thus it appears that the biogeographical limits for sustained cold-water coral growth along the NE Atlantic margin are strongly related to climate change. By focussing on the last glacial-interglacial cycle, this study shows that palaeo-productivity was increased during the last glacial. This was likely driven by the fertilisation effect of an increased input of aeolian dust and locally intensified upwelling. After the Younger Dryas cold event, the input of aeolian dust and productivity significantly decreased concurrent with an increase in water temperatures in the GoC. This primarily resulted in reduced food availability and caused a widespread demise of the formerly thriving coral ecosystems. Moreover, these climate induced changes most likely caused a latitudinal shift of areas withoptimum coral growth conditions towards the northern NE Atlantic where more suitable environmental conditions established with the onset of the Holocene. |
| title | Glacial cold-water coral: ages, isotope concentrations and ratios |
| topic | 64PE229; Age, relative; Age, standard deviation; Belgica area off Morocco; Center for Marine Environmental Sciences; Comment of event; Coral; DEPTH, sediment/rock; Event label; Faro/Almazan mud volcano; GAP; GC; GC25; GC27; GC35; GC36; GC44; GeoB9018-1; GeoB9031-1; GeoB9032-1; GeoB9070-1; Gravity corer; Gulf of Cádiz, Atlantic Ocean; HERMIONE; Hesperides mud volcano; Hotspot Ecosystem Research and Mans Impact On European Seas; Latitude of event; Longitude of event; M2004-02_PC; Maria S. Merian; MARUM; Moundforce 2004; MSM01/3; MSM01/3_254; MSM01/3_257; MSM01/3_292; MSM01/3_293; MSM01/3_325; PC; Pelagia; Piston corer; SO175; Sonne; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation; δ234 Uranium; δ234 Uranium, standard deviation |
| url | https://doi.org/10.1594/PANGAEA.770171 |