FN Archimer Export Format
PT J
TI Morphology and environment of cold-water coral carbonate mounds on the NW European margin
BT 
AF WHEELER, Andrew J.
   BEYER, A
   FREIWALD, A
   DE HAAS, H
   HUVENNE, V. A. I.
   KOZACHENKO, M
   OLU, Karine
   OPDERBECKE, Jan
AS 1:1;2:3;3:4;4:5;5:6;6:1;7:7;8:8;
FF 1:;2:;3:;4:;5:;6:;7:PDG-DOP-DCB-EEP-LEP;8:PDG-DOP-DCM-SM;
C1 Univ Coll Cork, Dept Geol, Cork, Ireland.
   Univ Coll Cork, Environm Res Inst, Cork, Ireland.
   Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany.
   Univ Erlangen Nurnberg, Inst Paleontol, D-91054 Erlangen, Germany.
   Royal Netherlands Inst Sea Res NIOZ, NL-1790 AB Den Burg, Netherlands.
   Univ Ghent, Renard Ctr Marine Geol, B-9000 Ghent, Belgium.
   IFREMER, Ctr Brest, F-29280 Plouzane, France.
   IFREMER, Underwater Robot, Navigat & Vis Dept, F-83507 La Seyne Sur Mer, France.
C2 UNIV COLL CORK (UCC), IRELAND
   UNIV COLL CORK (UCC), IRELAND
   INST A WEGENER, GERMANY
   UNIV ERLANGEN NURNBERG, GERMANY
   INST SEA RESEARCH (NIOZ), NETHERLANDS
   UNIV GHENT, BELGIUM
   IFREMER, FRANCE
   IFREMER, FRANCE
SI BREST
   TOULON
SE PDG-DOP-DCB-EEP-LEP
   PDG-DOP-DCM-SM
IN WOS Ifremer jusqu'en 2018
   copubli-europe
IF 1.719
TC 148
UR https://archimer.ifremer.fr/doc/2007/publication-2411.pdf
LA English
DT Article
CR CARACOLE
BO L'Atalante
DE ;Seabed mapping;Environmental setting;Morphology;Cold water coral;Carbonate mound
AB Cold-water coral carbonate mounds, owing their presence mainly to the framework building coral Lophelia pertusa and the activity of associated organisms, are common along the European margin with their spatial distribution allowing them to be divided into a number of mound provinces. Variation in mound attributes are explored via a series of case studies on mound provinces that have been the most intensely investigated: Belgica, Hovland, Pelagia, Logachev and Norwegian Mounds. Morphological variation between mound provinces is discussed under the premise that mound morphology is an expression of the environmental conditions under which mounds are initiated and grow. Cold-water coral carbonate mounds can be divided into those exhibiting "inherited" morphologies (where mound morphology reflects the morphology of the colonised features) and "developed" morphology (where the mounds assume their own gross morphology mainly reflecting dominant hydrodynamic controls). Finer-scale, surface morphological features mainly reflecting biological growth forms are also discussed.
PY 2007
PD FEB
SO International Journal of Earth Sciences
SN 1437-3254
PU Springer
VL 96
IS 1
UT 000243397100004
BP 37
EP 56
DI 10.1007/s00531-006-0130-6
ID 2411
ER

EF