A5013326071- Geology and Paleoclimatology Research
- Geological and Geophysical Studies
- Paleontology and Stratigraphy of Fossils
- Methane Hydrates and Related Phenomena
- Pacific and Southeast Asian Studies
- Coral and Marine Ecosystems Studies
- Geological formations and processes
- Seismic Imaging and Inversion Techniques
- Reservoir Engineering and Simulation Methods
- Drilling and Well Engineering
- Geophysics and Gravity Measurements
- Isotope Analysis in Ecology
- Geological and Geophysical Studies Worldwide
- Hydrocarbon exploration and reservoir analysis
- Marine animal studies overview
- Echinoderm biology and ecology
- Geomagnetism and Paleomagnetism Studies
- Marine Biology and Ecology Research
- Geological Modeling and Analysis
- Pleistocene-Era Hominins and Archaeology
- Microbial Community Ecology and Physiology
- earthquake and tectonic studies
- Hydraulic Fracturing and Reservoir Analysis
- Geological and Geochemical Analysis
- Marine and fisheries research
Centre de Recherche et d’Enseignement de Géosciences de l’Environnement
2015-2025
Collège de France
1991-2024
Aix-Marseille Université
2011-2024
Institut de Recherche pour le Développement
2010-2024
Centre National de la Recherche Scientifique
2011-2024
Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement
2020-2024
Sustainable Europe Research Institute
2017-2022
Beicip Franlab (France)
2015
Laboratoire Méditerranéen de Préhistoire Europe Afrique
2004-2014
University of Arizona
2013
Research Article| June 01, 1997 Continuous record of reef growth over the past 14 k.y. on mid-Pacific island Tahiti Lucien F. Montaggioni; Montaggioni 1Unité Associée au Centre National de la Recherche Scientifique no. 6019, Université Provence, 13331 Marseille Cedex 03, France Search for other works by this author on: GSW Google Scholar Guy Cabioch; Cabioch 2Institut Français pour le Développement en Coopération, B.P. 48, 06230 Villefranche-sur-Mer, Gilbert Camoin; Camoin 3Unité Mixte 132,...
Early Riser How glacial-interglacial cycles and the long-term variability of sea level depend on amount energy received by Earth from Sun is unclear. Thomas et al. (p. 1186 , published online 23 April; see cover) report results fossil corals found in Tahiti that indicate began to rise when insolation at 65° North latitude was near a minimum, not after it had begun rise, as predicted Milankovitch theory. In contrast, timing last deglaciation agrees well with Thus, glacial do behave simply...
Research Article| July 01, 2012 Reef response to sea-level and environmental changes during the last deglaciation: Integrated Ocean Drilling Program Expedition 310, Tahiti Sea Level Gilbert F. Camoin; Camoin * 1CEREGE, UMR 7330, CNRS-Université Paul Cézanne-Collège de France-IRD, B.P. 80, F-13545 Aix-en-Provence, cedex 4, France *E-mail: gcamoin@cerege.fr. Search for other works by this author on: GSW Google Scholar Claire Seard; Seard Pierre Deschamps; Deschamps Jody M. Webster; Webster...
Abstract There is considerable uncertainty about future sea‐level projections due to the current poor understanding of vulnerability and sensitivity ice sheets global warming. Fossil coral reefs represent a unique archive associated environmental changes that extend far beyond instrumental records. Here, recent advances in this field are summarized, focusing on periods Earth history typified by rapid rise short‐term climate excursions. Sea‐level reef response records from Last Deglaciation,...
Research Article| February 01, 1993 Stromatolites associated with coralgal communities in Holocene high-energy reefs Lucien F. Montaggioni; Montaggioni 1URA 1208 du Centre National de la Recherche Scientifique, Sédimentologie/Paléontologie, Université Provence, 13331 Marseille cedex 3, France2Centre l'Environnement, Muséum d'Histoire Naturelle, Ecole Pratique des Hautes Etudes, Moorea, French Polynesia Search for other works by this author on: GSW Google Scholar Gilbert Camoin France...
ABSTRACT Drill cores from Holocene reefs on Tahiti (French Polynesia) reveal a framework composed of massive branching acroporids encrusted by coralline algae associated with sessile vermetid gastropods and arborescent foraminifers. Laminated micritic crusts form coatings over coral branches or, more commonly, related encrusting organisms throughout the cored reef sections; these appear as major structural volumetric component framework. The microbial nature is inferred their typical organic...
Mid- to late-Holocene sea-level records from low-latitude regions serve as an important baseline of natural variability in sea level and global ice volume prior the Anthropocene. Here, we reconstruct a high-resolution curve encompassing last 6000 years based on comprehensive study coral microatolls, which are sensitive low-tide recorders. Our is microatolls several islands single region comprises total 82 index points. Assuming thermosteric contributions negligible millennial time scales,...
Abstract IODP Expedition 310 recovered more than 600 m of Post Last‐Glacial‐Maximum (LGM) coral reef framework rocks from the current tract surrounding island Tahiti. Six sites (12 holes) were sampled for paleomagnetic studies on south side island, termed Maraa tract, and five north Tiarei tract. The are ∼8,000–15,000 cal. YBP in age based 300 radiocarbon uranium‐series dates. We have inclination relative paleointensity records all these holes with an average sampling interval ∼100–200...
The International Ocean Drilling Programme (IODP3)After decades of unified international programmes, from DSDP to the Discovery Program that ended on 30 September 2024, post-2024 scientific ocean drilling initiatives will see a transition single programme operated by independent platform providers programmes.Through two-year long process exchange views and ambitions, ECORD Japan agreed build joint programme: - IODP3(IODP-cubed).IODP3 consists an collaboration addressing important questions...
Charles Darwin described in 1842 the island of Bora (Society Islands, Central South Pacific) as key example for a subsiding basaltic oceanic with related reef development. He recognized that lagoon developed between an outer barrier sand apron and inner fringing attached to shore volcanic island. In order quantify past sea-level paleoenvironmental changes subsidence, lagoonal sediments were cored 2024 context Bora2coring project. Previous shorter cores indicated Holocene are...