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The giant Mauritanian cold-water coral mound province: Oxygen control on coral mound formation

Wienberg, C. (författare)
Titschack, J. (författare)
Freiwald, A. (författare)
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Frank, N. (författare)
Lundälv, Tomas, 1944 (författare)
Gothenburg University,Göteborgs universitet,Havsmiljöinstitutet,Swedish Institute for the Marine Environment
Taviani, M. (författare)
Beuck, L. (författare)
Schroder-Ritzrau, A. (författare)
Krengel, T. (författare)
Hebbeln, D. (författare)
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 (creator_code:org_t)
Elsevier BV, 2018
2018
Engelska.
Ingår i: Quaternary Science Reviews. - : Elsevier BV. - 0277-3791. ; 185, s. 135-152
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https://doi.org/10.1...
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https://doi.org/10.1...
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  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The largest coherent cold-water coral (CWC) mound province in the Atlantic Ocean exists along the Mauritanian margin, where up to 100 m high mounds extend over a distance of similar to 400 km, arranged in two slope-parallel chains in 400-550 m water depth. Additionally, CWCs are present in the numerous submarine canyons with isolated coral mounds being developed on some canyon flanks. Seventy-seven Uranium-series coral ages were assessed to elucidate the timing of CWC colonisation and coral mound development along the Mauritanian margin for the last similar to 120,000 years. Our results show that CWCs were present on the mounds during the Last Interglacial, though in low numbers corresponding to coral mound aggradation rates of 16 cm kyr(-1). Most prolific periods for CWC growth are identified for the last glacial and deglaciation, resulting in enhanced mound aggradation (>1000 cm kyr(-1)), before mound formation stagnated along the entire margin with the onset of the Holocene. Until today, the Mauritanian mounds are in a dormant state with only scarce CWC growth. In the canyons, live CWCs are abundant since the Late Holocene at least. Thus, the canyons may serve as a refuge to CWCs potentially enabling the observed modest re-colonisation pulse on the mounds along the open slope. The timing and rate of the pre-Holocene coral mound aggradation, and the cessation of mound formation varied between the individual mounds, which was likely the consequence of vertical/lateral changes in water mass structure that placed the mounds near or out of oxygen-depleted waters, respectively. (C) 2018 The Authors. Published by Elsevier Ltd.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)
NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)

Nyckelord

Lophelia pertusa
Coral mound
Submarine canyon
Uranium-series dating
Mound aggradation rate
lophelia-pertusa scleractinia
deep-sea corals
covered carbonate mound
rockall trough margin
mingulay reef complex
last glacial maximum
ne
Atlantic-Ocean
Gulf-of-Mexico
Northeast Atlantic
Northwest Africa

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