FN Archimer Export Format
PT J
TI Impact of Late Quaternary climatic fluctuations on coastal systems: Evidence from high-resolution geophysical, sedimentological and geochronological data from the Java Island
BT 
AF NOVICO, Franto
   MENIER, David
   MATHEW, Manoj
   RAMKUMAR, Mu
   SANTOSH, M.
   ENDYANA, Cipta
   DEWI, Kresna Tri
   KURNIAWAN, Indra
   LAMBERT, Clement
   GOUBERT, Evelyne
AS 1:1,2;2:3;3:4;4:5;5:6,7;6:1;7:8;8:9;9:3;10:3;11:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;
C1 Department of Engineering Geology, Padjadjaran University, 45363, Jatinangor, Indonesia
   Marine Geological Research and Development Center, Ministry of Energy and Mineral Resources, 40174, Bandung, Indonesia
   Laboratoire Géoscience Océan, UMR CNRS 6538, Université Bretagne Sud, 56017, Vannes, France
   Laboratoire Géoscience Océan, UMR CNRS/UBO/UBS 6538, IUEM, Université de Brest, 29280, Plouzané, France
   Department of Geology, Periyar University, 636011, Salem, India
   Department of Earth Sciences, University of Adelaide, Adelaide, SA, 5005, Australia
   Beijing School of Earth Sciences and Resources, China University of Geosciences, 100083, Beijing, China
   Center of Geological Survey, Ministry of Energy and Mineral Resources, 40122, Bandung, Indonesia
   Directorate of Water Resources, Ministry of Public Works and Housing, 12110, Jakarta, Indonesia
C2 UNIV PADJADJARAN, INDONESIA
   MINIST ENERGY & MINERAL RESOURCES, INDONESIA
   UBS, FRANCE
   UBO, FRANCE
   UNIV PERIYAR, INDIA
   UNIV ADELAIDE, AUSTRALIA
   UNIV CHINA GEOSCI, CHINA
   MINIST ENERGY & MINERAL RESOURCES, INDONESIA
   MINIST PUBL WORKS & HOUSING, INDONESIA
UM GEO-OCEAN
IN WOS Cotutelle UMR
   copubli-int-hors-europe
   copubli-sud
IF 4.2
TC 1
UR https://archimer.ifremer.fr/doc/00865/97716/106921.pdf
LA English
DT Article
DE ;Last glacial maximum;Java sea;Incised valleys;Depositional controls;Stratal morphology
AB The major climatic oscillations during the Quaternary Period significantly influenced the evolution and distribution of ancient and modern coastal systems. Here we investigate the morphology and sedimentary infilling of submerged Late Quaternary incised valleys along the northern coast of Java Island (Indonesia) using highresolution geophysical, sedimentological and geochronological data. Our results indicate that the spatial development and morphology of the incised valleys are predominantly controlled by Quaternary glacial-interglacial eustatic fluctuations, within a marked subsiding setting. The valleys were incised during prominent Quaternary lowstands and most of the valley fill was emplaced during the last postglacial sea level rise. The valley fill forms a transgressive succession, consisting mainly of fluvial deposits at the base (possibly amalgamated from older sequences) overlain by shallow marine sediments and capped by hemipelagic deposits. The valley-fill architecture is strongly dependent on the valley morphology (depth of incision, width of the valleys, and extent of the intertidal zone). The shallow marine deposits contained within the narrow and linear valleys are mostly aggrading muds. The vertical incision and valley formation was chiefly controlled by the extent of glacial sea-level fluctuations. The studied sections represent the continental-offshore extension of a paleodeltaic system. The implication of our work is that even in predominantly enclosed shallow marine systems that are located distal to the shelf break, the response of the sedimentary system and ensuing stratigraphic configuration can be effectively impacted by the rapid and abrupt Quaternary global climatic transition and eustatic sea-level fluctuations. 
PY 2022
PD FEB
SO Marine And Petroleum Geology
SN 0264-8172
PU Elsevier Sci Ltd
VL 136
UT 000748975500001
DI 10.1016/j.marpetgeo.2021.105399
ID 97716
ER

EF