FN Archimer Export Format
PT J
TI A Late Quaternary record of highstand shedding from an isolated carbonate platform (Juan de Nova, southern Indian Ocean)
BT 
AF Counts, John
   Jorry, Stephan
   Vazquez riveiros, Natalia
   Jouet, Gwenael
   Giraudeau, Jacques
   Cheron, Sandrine
   Boissier, Audrey
   MIRAMONTES, Elda
AS 1:1,2;2:2;3:2;4:2;5:3;6:2;7:2;8:4;
FF 1:;2:PDG-REM-GM-LGS;3:PDG-REM-GM-LGS;4:PDG-REM-GM-LGS;5:;6:PDG-REM-GM-LCG;7:PDG-REM-GM-LCG;8:;
C1 Irish Centre for Research in Applied Geosciences (iCRAG); O'Brien Centre for Science, University College Dublin; Belfield Dublin 4 Ireland
   IFREMER; Unité Géosciences Marines - Pointe du Diable; 29280 Plouzané France
   UMR CNRS 5805 EPOC; Université de Bordeaux; Allée Geoffroy Saint-Hilaire; CS 50023 33615 Pessac Cedex France
   CNRS, UMR6538, Laboratoire Géosciences Océan; Institute Universitaire Européen de la Mer - Université de Bretagne Occidentale (IUEM-UBO); 29280 Plouzané France
C2 UNIV COLL DUBLIN, IRELAND
   IFREMER, FRANCE
   UNIV BORDEAUX, FRANCE
   CNRS, FRANCE
SI BREST
SE PDG-REM-GM-LGS
   PDG-REM-GM-LCG
UM LGO
IN WOS Ifremer UPR
   DOAJ
   copubli-france
   copubli-europe
   copubli-univ-france
IF 2.492
TC 11
UR https://archimer.ifremer.fr/doc/00474/58553/61108.pdf
   https://archimer.ifremer.fr/doc/00474/58553/61109.xlsx
LA English
DT Article
CR PAMELA-MOZ04
   PTOLEMEE
BO Pourquoi pas ?
   L'Atalante
DE ;aragonite;atoll;MIS 11;Mozambique Channel;sea-level change
AB A 27 m core collected on the seafloor near Juan de Nova island at 1909 m depth in the SW Indian Ocean preserves a high‐resolution record of carbonate sediment export to the deep sea over the past 1 Myr. Core chronology was established using calcareous nannofossil biostratigraphy and benthic foraminiferal δ18O. Throughout the core, preserved highstand intervals (MIS 1, 5, 7, 9, 11, 13, 15, 23 and 25) are marked by an increase in the aragonite content within the sediment. Aragonite is likely sourced from the nearby Juan de Nova carbonate platform ~10 km to the south, and is interpreted to result from flooding of the platform top. Platform inundation allows carbonate muds to be winnowed from their original shallow‐water environment of deposition, suspended in the water column, and redeposited onto the proximal slopes and within the basin. Sharp increases in aragonite content at the beginning of each highstand interval can be used to estimate the approximate sea‐level range when platform flooding occurred; results show that the depth of the platform top has likely changed little over the past 1 Myr due to balanced aggradation and subsidence. Previously hypothesized large‐scale aragonite dissolution cycles are evidenced by a disproportionally low aragonite increase during MIS 11. This study provides a new, exceptionally long record of highstand shedding, expanding the known occurrences of the process to the southern Indian Ocean and supporting its importance as a globally significant depositional mechanism that impacts deep‐sea stratigraphic records. 
PY 2019
PD SEP
SO Depositional Record
SN 2055-4877
PU Wiley
VL 5
IS 3
UT 000487658300011
BP 540
EP 557
DI 10.1002/dep2.57
ID 58553
ER

EF