scholarly journals Cold-water coral reef frameworks, megafaunal communities and evidence for coral carbonate mounds on the Hatton Bank, north east Atlantic

Facies ◽  
2008 ◽  
Vol 54 (4) ◽  
pp. 621-621
Author(s):  
J. M. Roberts ◽  
L.-A. Henry ◽  
D. Long ◽  
J. P. Hartley
2019 ◽  
Vol 6 ◽  
Author(s):  
Evert de Froe ◽  
Lorenzo Rovelli ◽  
Ronnie N. Glud ◽  
Sandra R. Maier ◽  
Gerard Duineveld ◽  
...  

2013 ◽  
Vol 95 (7) ◽  
pp. 1461-1474 ◽  
Author(s):  
R.W.M. van Soest ◽  
N.J. de Voogd

A comparison is made of sponge diversity and abundance in nine cold-water coral reef locations situated in four regions of the north-east Atlantic, Rockall Bank (two reef locations, both deep, oceanic), Porcupine Bank (two locations, both deep, oceanic), Mingulay (two reef locations, both shallow, near-shore), Skagerrak (three reef locations, all shallow, near-shore). Literature data from two reefs were used to supplement our own data from seven reef locations. Geographical distance between the regions may be summarized as Rockall Bank < Porcupine << Mingulay <<< Skagerrak. The first three regions are all situated west of the British Isles, and prevailing current patterns and bottom conditions would make direct larval transport between all three a distinct possibility. The fourth region, Skagerrak, is situated away from the Atlantic regions, with larval contact hampered by long distances over predominantly shallow sedimented sea bottoms. Accordingly, we expected the largest taxon turnover to be between the three Atlantic regions and the Skagerrak localities. However, cluster analysis and multidimensional scaling clearly show, that shelf reefs at Mingulay were faunistically closer to the geographically- distant shelf reefs at Skagerrak than to the geographically closer bathyal reefs of the Porcupine–Rockall area. Further research is necessary to determine whether depth is a proxy for other abiotic factors such as oceanic circulation or trophic conditions.


2013 ◽  
Vol 375 ◽  
pp. 176-187 ◽  
Author(s):  
Mélanie Douarin ◽  
Mary Elliot ◽  
Stephen R. Noble ◽  
Daniel Sinclair ◽  
Lea-Anne Henry ◽  
...  

2016 ◽  
Vol 31 (3) ◽  
pp. 365-379 ◽  
Author(s):  
Andres Rüggeberg ◽  
Sascha Flögel ◽  
Wolf-Christian Dullo ◽  
Jacek Raddatz ◽  
Volker Liebetrau

2006 ◽  
Vol 96 (1) ◽  
pp. 37-56 ◽  
Author(s):  
A. J. Wheeler ◽  
A. Beyer ◽  
A. Freiwald ◽  
H. de Haas ◽  
V. A. I. Huvenne ◽  
...  

2019 ◽  
Vol 8 (1) ◽  
pp. 40 ◽  
Author(s):  
Alexandra Jarna ◽  
Nicole J. Baeten ◽  
Sigrid Elvenes ◽  
Valérie K. Bellec ◽  
Terje Thorsnes ◽  
...  

Cold-water coral reefs are hotspots of biological diversity and play an important role as carbonate factories in the global carbon cycle. Reef-building corals can be found in cold oceanic waters around the world. Detailed knowledge on the spatial location and distribution of coral reefs is of importance for spatial management, conservation and science. Carbonate mounds (reefs) are readily identifiable in high-resolution multibeam echosounder data but systematic mapping programs have relied mostly on visual interpretation and manual digitizing so far. Developing more automated methods will help to reduce the time spent on this laborious task and will additionally lead to more objective and reproducible results. In this paper, we present an attempt at testing whether rule-based classification can replace manual mapping when mapping cold-water coral carbonate mounds. To that end, we have estimated and compared the accuracies of manual mapping, pixel-based terrain analysis and object-based image analysis. To verify the mapping results, we created a reference dataset of presence/absence points agreed upon by three mapping experts. There were no statistically significant differences in the overall accuracies of the maps produced by the three approaches. We conclude that semi-automated rule-based methods might be a viable option for mapping carbonate mounds with high spatial detail over large areas.


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