FN Archimer Export Format
PT J
TI The community structure of deep-sea macrofauna associated with polymetallic nodules in the eastern part of the Clarion-Clipperton fracture zone
BT 
AF DE SMET, Bart
   PAPE, Ellen
   RIEHL, Torben
   BONIFACIO, Paulo
   COLSON, Liesbet
   VANREUSEL, Ann
AS 1:1;2:1;3:1,2;4:3;5:1;6:1;
FF 1:;2:;3:;4:PDG-REM-EEP-LEP;5:;6:;
C1 Ghent University, Belgium
   University of Hamburg, Germany
   IFREMER, Inst Carnot, EDROME, Ctr Bretagne,REM EEP,Lab Environm Profond, Plouzane, France
C2 UNIV GHENT, BELGIUM
   UNIV HAMBURG, GERMANY
   IFREMER, FRANCE
SI BREST
SE PDG-REM-EEP-LEP
IN WOS Ifremer jusqu'en 2018
   DOAJ
   copubli-europe
IF 5.247
TC 57
UR https://archimer.ifremer.fr/doc/00378/48885/49311.pdf
   https://archimer.ifremer.fr/doc/00378/48885/49312.pdf
   https://archimer.ifremer.fr/doc/00378/48885/49313.pdf
   https://archimer.ifremer.fr/doc/00378/48885/49314.pdf
   https://archimer.ifremer.fr/doc/00378/48885/49315.pdf
LA English
DT Article
DE ;polymetallic nodules;macrofauna;deep sea;CCFZ;biodiversity;community structure;deep-sea mining
AB Deep-sea areas characterized by the presence of polymetallic nodules are getting increased attention due to their potential commercial and strategic interest for metals such as nickel, copper and cobalt. The polymetallic nodules occur in areas beyond national jurisdiction, regulated by the International Seabed Authority (ISA). Under exploration contracts, contractors have the obligation to determine the environmental baseline in the exploration areas. Despite a large number of scientific cruises to the central east Pacific Ocean, few published data on the macrofaunal biodiversity and community structure are available for the abyssal fields of the Clarion-Clipperton Fracture Zone (CCFZ). This study focused on the macrofaunal abundance, diversity and community structure in three physically comparable, mineable sites located in the license area of Global Sea Mineral Resources N.V., at ~ 4500 m depth. A homogeneous but diverse macrofaunal community associated with the sediment from polymetallic nodule areas was observed at a scale of 10s to 100s of km. However, slight differences in the abundance and diversity of Polychaeta between sites can be explained by a decline in the estimated flux of particulate organic carbon (POC) along a southeast-northwest gradient, as well as by small differences in sediment characteristics and nodule abundance. The observed homogeneity in the macrofaunal community is an important prerequisite for assigning areas for impact and preservation reference zones. However, a precautionary approach regarding mining activities is recommended, awaiting further research during the exploration phase on environmental factors structuring macrofaunal communities in the CCFZ. For instance, future studies should consider habitat heterogeneity, which was previously shown to structure macrofauna communities at larger spatial scales. Acknowledging the limited sampling in the current study, a large fraction (59-85%; depending on the richness estimator used and the macrofaunal taxon of interest) of the macrofaunal genus/species diversity from the habitat under study was characterized. 
PY 2017
SO Frontiers In Marine Science
SN 2296-7745
PU Frontiers Media SA
VL 4
IS 103
UT 000457690600103
DI 10.3389/fmars.2017.00103
ID 48885
ER

EF