scholarly journals Feedbacks between hydrodynamics and cold-water coral mound development

2021 ◽  
Vol 178 ◽  
pp. 103641
Author(s):  
Anna-Selma van der Kaaden ◽  
Christian Mohn ◽  
Theo Gerkema ◽  
Sandra R. Maier ◽  
Evert de Froe ◽  
...  
Keyword(s):  
Cold Water ◽  
Water Coral

Predicting suitable habitat for the cold-water coral Lophelia pertusa (Scleractinia)

2008 ◽  
Vol 55 (8) ◽  
pp. 1048-1062 ◽  
Author(s):  
Andrew J. Davies ◽  
Max Wisshak ◽  
James C. Orr ◽  
J. Murray Roberts
Keyword(s):  
Cold Water ◽  
Suitable Habitat ◽  
Lophelia Pertusa ◽  
Water Coral

scholarly journals Living benthic foraminifera from cold-water coral ecosystems in the eastern Alboran Sea, Western Mediterranean

Heliyon ◽  
2021 ◽  
pp. e07880
Author(s):  
Claudio Stalder ◽  
Akram El Kateb ◽  
Jorge E. Spangenberg ◽  
Loubna Terhzaz ◽  
Agostina Vertino ◽  
...  
Keyword(s):  
Benthic Foraminifera ◽  
Cold Water ◽  
Western Mediterranean ◽  
Alboran Sea ◽  
Alborán Sea ◽  
Water Coral

scholarly journals Seabed mapping for selecting cold-water coral protection areas on Hatton Bank, Northeast Atlantic

2009 ◽  
Vol 66 (9) ◽  
pp. 2013-2025 ◽  
Author(s):  
P. Durán Muñoz ◽  
M. Sayago-Gil ◽  
J. Cristobo ◽  
S. Parra ◽  
A. Serrano ◽  
...  
Keyword(s):  
Deep Sea ◽  
Ad Hoc ◽  
Cold Water ◽  
Interdisciplinary Approach ◽  
Western Slope ◽  
Northeast Atlantic ◽  
Fisheries Science ◽  
Seabed Mapping ◽  
Del Rio ◽  
Water Coral

Abstract Durán Muñoz, P., Sayago-Gil, M., Cristobo, J., Parra, S., Serrano, A., Díaz del Rio, V., Patrocinio, T., Sacau, M., Murillo, F. J., Palomino, D., and Fernández-Salas, L. M. 2009. Seabed mapping for selecting cold-water coral protection areas on Hatton Bank, Northeast Atlantic. – ICES Journal of Marine Science, 66: 2013–2025. Research into vulnerable marine ecosystems (VMEs) on the high seas and the impacts of bottom fishing and ad hoc management measures are high priority today thanks to UN General Assembly Resolution 61/105. An interdisciplinary methodology (specifically designed for selecting cold-water coral protection areas) and a case study focused on the Hatton Bank (NE Atlantic) are presented. This interdisciplinary approach, developed under the ECOVUL/ARPA project, was based on conventional fisheries science, geomorphology, benthic ecology, and sedimentology. It contributes to defining practical criteria for identifying VMEs, to improving knowledge of their distribution off Europe's continental shelf, and to providing advice on negative fishing impacts and habitat protection. The approach was used to identify the bottom-trawl deep-sea fishery footprint on the western slope of Hatton Bank, to map the main fishing grounds and related deep-sea habitats (1000–1500 m deep), and to study the interactions between fisheries and cold-water corals. The results lead to a proposal to close the outcrop area (4645 km2) located on the western slope of Hatton Bank as a conservation measure for cold-water corals.

The “Sardinian cold-water coral province” in the context of the Mediterranean coral ecosystems

2017 ◽  
Vol 145 ◽  
pp. 61-78 ◽  
Author(s):  
M. Taviani ◽  
L. Angeletti ◽  
S. Canese ◽  
R. Cannas ◽  
F. Cardone ◽  
...  
Keyword(s):  
Cold Water ◽  
The Mediterranean ◽  
Water Coral

scholarly journals Willingness to pay for unfamiliar public goods: Preserving cold-water coral in Norway

2015 ◽  
Vol 112 ◽  
pp. 53-67 ◽  
Author(s):  
Margrethe Aanesen ◽  
Claire Armstrong ◽  
Mikołaj Czajkowski ◽  
Jannike Falk-Petersen ◽  
Nick Hanley ◽  
...  
Keyword(s):  
Willingness To Pay ◽  
Public Goods ◽  
Cold Water ◽  
Water Coral

scholarly journals Involving fishers in scaling up the restoration of cold-water coral gardens on the Mediterranean continental shelf

2021 ◽  
Vol 262 ◽  
pp. 109301
Author(s):  
Maria Montseny ◽  
Cristina Linares ◽  
Núria Viladrich ◽  
Marina Biel ◽  
Nuno Gracias ◽  
...  
Keyword(s):  
Continental Shelf ◽  
Cold Water ◽  
Scaling Up ◽  
The Mediterranean ◽  
Water Coral

The sediment composition and predictive mapping of facies on the Propeller Mound—A cold-water coral mound (Porcupine Seabight, NE Atlantic)

2010 ◽  
Vol 30 (17) ◽  
pp. 1814-1829 ◽  
Author(s):  
Katrin Heindel ◽  
Jürgen Titschack ◽  
Boris Dorschel ◽  
Veerle A.I. Huvenne ◽  
André Freiwald
Keyword(s):  
Cold Water ◽  
Ne Atlantic ◽  
Sediment Composition ◽  
Predictive Mapping ◽  
Porcupine Seabight ◽  
Water Coral

scholarly journals <sup>210</sup>Pb-<sup>226</sup>Ra chronology reveals rapid growth rate of <i>Madrepora oculata</i> and <i>Lophelia pertusa</i> on world's largest cold-water coral reef

2012 ◽  
Vol 9 (3) ◽  
pp. 1253-1265 ◽  
Author(s):  
P. Sabatier ◽  
J.-L. Reyss ◽  
J. M. Hall-Spencer ◽  
C. Colin ◽  
N. Frank ◽  
...  
Keyword(s):  
Growth Rate ◽  
Coral Reef ◽  
Metal Oxides ◽  
Growth Rates ◽  
Cold Water ◽  
Age And Growth ◽  
Lophelia Pertusa ◽  
Fe Oxide ◽  
Oxide Contamination ◽  
Water Coral

Abstract. Here we show the use of the 210Pb-226Ra excess method to determine the growth rate of two corals from the world's largest known cold-water coral reef, Røst Reef, north of the Arctic circle off Norway. Colonies of each of the two species that build the reef, Lophelia pertusa and Madrepora oculata, were collected alive at 350 m depth using a submersible. Pb and Ra isotopes were measured along the major growth axis of both specimens using low level alpha and gamma spectrometry and trace element compositions were studied. 210Pb and 226Ra differ in the way they are incorporated into coral skeletons. Hence, to assess growth rates, we considered the exponential decrease of initially incorporated 210Pb, as well as the increase in 210Pb from the decay of 226Ra and contamination with 210Pb associated with Mn-Fe coatings that we were unable to remove completely from the oldest parts of the skeletons. 226Ra activity was similar in both coral species, so, assuming constant uptake of 210Pb through time, we used the 210Pb-226Ra chronology to calculate growth rates. The 45.5 cm long branch of M. oculata was 31 yr with an average linear growth rate of 14.4 ± 1.1 mm yr−1 (2.6 polyps per year). Despite cleaning, a correction for Mn-Fe oxide contamination was required for the oldest part of the colony; this correction corroborated our radiocarbon date of 40 yr and a mean growth rate of 2 polyps yr−1. This rate is similar to the one obtained in aquarium experiments under optimal growth conditions. For the 80 cm-long L. pertusa colony, metal-oxide contamination remained in both the middle and basal part of the coral skeleton despite cleaning, inhibiting similar age and growth rate estimates. The youngest part of the colony was free of metal oxides and this 15 cm section had an estimated a growth rate of 8 mm yr−1, with high uncertainty (~1 polyp every two to three years). We are less certain of this 210Pb growth rate estimate which is within the lowermost ranges of previous growth rate estimates. We show that 210Pb-226Ra dating can be successfully applied to determine the age and growth rate of framework-forming cold-water corals if Mn-Fe oxide deposits can be removed. Where metal oxides can be removed, large M. oculata and L. pertusa skeletons provide archives for studies of intermediate water masses with an up to annual time resolution and spanning over many decades.

scholarly journals Opportunistic feeding on various organic food sources by the cold-water coral <i>Lophelia pertusa</i>

2014 ◽  
Vol 11 (1) ◽  
pp. 123-133 ◽  
Author(s):  
C. E. Mueller ◽  
A. I. Larsson ◽  
B. Veuger ◽  
J. J. Middelburg ◽  
D. van Oevelen
Keyword(s):  
Amino Acids ◽  
Fatty Acids ◽  
De Novo ◽  
Cold Water ◽  
Feeding Strategy ◽  
Food Sources ◽  
Coral Tissue ◽  
Lophelia Pertusa ◽  
Opportunistic Feeding ◽  
Water Coral

Abstract. The ability of the cold-water coral Lophelia pertusa to exploit different food sources was investigated under standardized conditions in a flume. The tested food sources, dissolved organic matter (DOM, added as dissolved free amino acids), bacteria, algae, and zooplankton (Artemia) were deliberately enriched in 13C and 15N. The incorporation of 13C and 15N was traced into bulk tissue, fatty acids, hydrolysable amino acids, and the skeleton (13C only) of L. pertusa. Incorporation rates of carbon (ranging from 0.8–2.4 μg C g−1 DW d–1) and nitrogen (0.2–0.8 μg N g−1 DW d–1) into coral tissue did not differ significantly among food sources indicating an opportunistic feeding strategy. Although total food assimilation was comparable among sources, subsequent food processing was dependent on the type of food source ingested and recovery of assimilated C in tissue compounds ranged from 17% (algae) to 35% (Artemia). De novo synthesis of individual fatty acids by L. pertusa occurred in all treatments as indicated by the 13C enrichment of individual phospholipid-derived fatty acids (PLFAs) in the coral that were absent in the added food sources. This indicates that the coral might be less dependent on its diet as a source of specific fatty acids than expected, with direct consequences for the interpretation of in situ observations on coral nutrition based on lipid profiles.

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