Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Doug G. Masson"'
Autor:
Veerle A I Huvenne, Paul A Tyler, Doug G Masson, Elizabeth H Fisher, Chris Hauton, Veit Hühnerbach, Timothy P Le Bas, George A Wolff
Publikováno v:
PLoS ONE, Vol 6, Iss 12, p e28755 (2011)
Cold-water corals are azooxanthellate species found throughout the ocean at water depths down to 5000 m. They occur in patches, reefs or large mound structures up to 380 m high, and as ecosystem engineers create important habitats for a diverse fauna
Externí odkaz:
https://doaj.org/article/339be6abb5fb412fa79a61399ca063dd
Autor:
Doug G. Masson, Henry A. Ruhl, Antonina Rogacheva, Paul A. Tyler, Elizabeth J. Ross, David S.M. Billett, Chrysoula Gubili, Chris Hauton, Charalampos Tsairidis, Andrew Yool
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 137:288-296
Despite the plethora of studies on swallow-water invertebrates, almost nothing is known about the evolution and population structure of deep-sea species at the global scale. The aim of this study was to assess phylogeographic patterns of a common and
Publikováno v:
Quaternary Science Reviews. 72:63-82
Large submarine landslides can have serious socioeconomic consequences as they have the potential to cause tsunamis and damage seabed infrastructure. It is important to understand the frequency of these landslides, and how that frequency is related t
Publikováno v:
Geology. 40:11-14
Publikováno v:
Sedimentology. 55:1875-1887
The Darwin Mounds are small (up to 70 m in diameter), discrete cold-water coral banks found at c. 950 m water depth in the northern Rockall Trough, north-east Atlantic. Formerly described in terms of their genesis, the Darwin Mounds are re-evaluated
Publikováno v:
Marine Geology (0025-3227) (Elsevier), 2006-12, Vol. 234, N. 1-4, P. 261-270
The late Holocene mud wedge on the Adriatic shelf offshore Ortona, Italy, shows undulating sub-parallel seismic reflector sequences which extend several kilometres along strike and 100200 m down-dip in water depth between 20 and 80 m. The amplitude
Autor:
Atle Nygård, Doug G. Masson, Hans Petter Sejrup, K. Berg, Petter Bryn, R. Lien, Haflidi Haflidason, Jürgen Mienert, Carl Fredrik Forsberg
Publikováno v:
Marine Geology. 213:201-234
The detailed mapping of the Storegga Slide morphological elements and the analyses of the slide development are based on high-quality acoustic and sampling data sets acquired through a cooperation between academia and the petroleum industry. The Stor
Publikováno v:
Marine Geology. 192:215-237
Four types of large-scale sediment bedform occur in the northeast Rockall Trough: broad sheeted drifts, elongate drifts, sediment waves and thin contourite sheets. A large sheeted drift occupies the northern basin; its crest can be traced for 40 km p
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography
The deep-sea floor occupies about 60% of the surface of the planet and is covered mainly by fine sediments. Most studies of deep-sea benthic fauna therefore have concentrated on soft sediments with little sampling of hard substrata, such as rocky out
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7d7b1c970f5c1bfa03bfda15dc41ac3
Publikováno v:
Submarine Mass Movements and Their Consequences., ed. by Yamada, Y., Kawamura, K., Ikehara, K., Ogawa, Y., Urgeles, R., Mosher, D., Chaytor, J. and Strasser, M. Advances in Natural and Technological Hazards Research, 31 . Springer, Dordrecht, Netherlands, pp. 277-287. ISBN 978-94-007-2161-6
Submarine Mass Movements and Their Consequences ISBN: 9789400721616
Submarine Mass Movements and Their Consequences ISBN: 9789400721616
Overpressure generation due to rapid sediment deposition can result in low effective stresses within the sediment column. It has been proposed that these large overpressures are the main preconditioning factor for causing large-scale submarine slope
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e65cb236efabe8f35644ac5f2d3dcf56
http://oceanrep.geomar.de/43262/
http://oceanrep.geomar.de/43262/