FN Archimer Export Format
PT J
TI Staggered cold-water coral mound build-up on an Alboran ridge during the last deglacial (East Melilla Mound Field, western Mediterranean)
BT 
AF Fentimen, Robin
   Feenstra, Eline J.
   Rüggeberg, Andres
   Hall, Efraim
   Rosso, Antonietta
   Hajdas, Irka
   Jaramillo-Vogel, David
   Grobéty, Bernard
   Adatte, Thierry
   Van Rooij, David
   Frank, Norbert
   Foubert, Anneleen
AS 1:1;2:1;3:1;4:1;5:2;6:3;7:1;8:1;9:4;10:5;11:6;12:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;
C1 Department of Geosciences, University of Fribourg, Chemin du Musée 6, Fribourg, Switzerland
   Department of Biological, Geological and Environmental Sciences, University of Catania, Catania, Italy
   Laboratory of Ion Beam Physics, ETH Zurich, Otto-Stem-Weg 5, Zurich CH-8093, Switzerland
   Institute of Earth Surface Dynamics, University of Lausanne, Lausanne, Switzerland
   Department of Geology, Ghent University, Krijgslaan 281 S8, B9000, Gent, Belgium
   Institute of Environmental Physics, University of Heidelberg, Im Neuenheimer Feld 229, Heidelberg 69120, Germany
C2 UNIV FRIBOURG, SWITZERLAND
   UNIV CATANIA, ITALY
   ETH ZURICH, SWITZERLAND
   UNIV LAUSANNE, SWITZERLAND
   UNIV GHENT, BELGIUM
   UNIV HEIDELBERG, GERMANY
IF 2.9
TC 0
UR https://archimer.ifremer.fr/doc/00821/93275/99933.pdf
LA English
DT Article
CR MD 194 / EUROFLEET - GATEWAY
BO Marion Dufresne
DE ;Cold -water corals;Mediterranean Sea;B ?lling-Aller ?d;Holocene;Benthic foraminifera;Palaeoclimate
AB The start-up, build-up and demise of cold-water coral mounds are governed by environmental changes at global, regional and local scales. Whilst the formation of cold-water coral mounds across the globe is widely documented to follow interglacial-glacial cycles, less is known about their response to local environmental fluctuations during short time intervals. This study investigates the local variations in coral mound build-up along Brittlestar Ridge I (East Melilla Coral Province, Southeast Alboran Sea) by comparing three on-mound gravity cores collected ∼1 km apart, together with five previously described on-mound records, along a longitudinal transect on the ridge crest. Radiocarbon foraminiferal dating associated to U-series coral dating allowed to correlate the different records and to estimate mound aggradation rates, whilst grain-size analysis provided information on bottom current velocities. Prior to a rapid period of coral mound build-up initiated at ∼14.75 ka BP, the three cores present an occurrence of cm-thick bryozoan-dominated intervals nearly entirely consisting of the erect cheleistome Buskea dichotoma. Offsets between benthic foraminiferal and coral ages suggest that older dead allochtonous benthic foraminifera are possibly eroded from neighbouring settings, transported and deposited within the coral framework. In contrast, younger benthic foraminifera would develop on dead coral framework during periods of reef stagnation. The comparison of all cores indicates that mound build-up along the ridge did not follow the same timing during the last ∼16 kyr and that mound aggradation was marked by a staggered dynamic. Both local differences in bottom current velocities and patchiness of other key environmental actors (e.g. substrate availability) are suspected to drive the observed staggered mound build-up. Cold-water coral mound build-up shows important differences during Greenland Interstadial 1 (i.e. the Bølling-Allerød) and the Holocene, hence examplifying how local environmental variability may overprint global and regional climate variability over short time periods. 
PY 2023
PD MAR
SO Marine Geology
SN 0025-3227
PU Elsevier BV
VL 457
UT 000946730300001
DI 10.1016/j.margeo.2023.106994
ID 93275
ER

EF