The mineralogic and isotopic fingerprint of equatorial carbonates: Kepulauan Seribu, Indonesia

Kepulauan Seribu is an isolated patch reef complex situated in the Java Sea (Indonesia) and is a typical example for a humid, equatorial carbonate system. We investigate the mineralogical and isotopic fingerprint of Panggang, one of the reef platforms of Kepulauan Seribu, to evaluate differences to...

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Bibliographic Details
Published in:International journal of earth sciences : Geologische Rundschau 2021-03, Vol.110 (2), p.513-534
Main Authors: Utami, Dwi Amanda, Reuning, Lars, Hallenberger, Maximillian, Cahyarini, Sri Yudawati
Format: Article
Language:English
Subjects:
Abundance
Algae
Aquatic plants
Atmospheric convection
Carbonates
Catchment area
Catchments
Depletion
Earth and Environmental Science
Earth Sciences
Equatorial regions
Fingerprints
Fluvial sediments
Freshwater
Geochemistry
Geology
Geophysics/Geodesy
High temperature
Inland water environment
Isotopes
Mangroves
Mineral Resources
Minerals
Mollusks
Original Paper
Relative abundance
River catchments
River discharge
River flow
River runoff
Rivers
Runoff
Sedimentology
Sediments
Shallow water
Structural Geology
Turbidity
Water temperature
Work platforms
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Summary:Kepulauan Seribu is an isolated patch reef complex situated in the Java Sea (Indonesia) and is a typical example for a humid, equatorial carbonate system. We investigate the mineralogical and isotopic fingerprint of Panggang, one of the reef platforms of Kepulauan Seribu, to evaluate differences to other carbonate systems, using isotope in combination with XRD and SEM analysis. A characteristic property of shallow water (
ISSN:1437-3254
1437-3262
DOI:10.1007/s00531-020-01968-9