Intertwined effects of climate and land use change on environmental dynamics and carbon accumulation in a mangrove-fringed coastal lagoon in Java, Indonesia.

XRF carbon accumulation rate climate change estuary land use change mangrove palaeoecology watershed

Journal

Global change biology
ISSN: 1365-2486
Titre abrégé: Glob Chang Biol
Pays: England
ID NLM: 9888746

Informations de publication

Date de publication:
03 2020
Historique:
received: 21 02 2019
accepted: 01 11 2019
pubmed: 11 12 2019
medline: 20 3 2020
entrez: 11 12 2019
Statut: ppublish

Résumé

The identification and quantification of natural carbon (C) sinks is critical to global climate change mitigation efforts. Tropical coastal wetlands are considered important in this context, yet knowledge of their dynamics and quantitative data are still scarce. In order to quantify the C accumulation rate and understand how it is influenced by land use and climate change, a palaeoecological study was conducted in the mangrove-fringed Segara Anakan Lagoon (SAL) in Java, Indonesia. A sediment core was age-dated and analyzed for its pollen and spore, elemental and biogeochemical compositions. The results indicate that environmental dynamics in the SAL and its C accumulation over the past 400 years were controlled mainly by climate oscillations and anthropogenic activities. The interaction of these two factors changed the lagoon's sediment supply and salinity, which consequently altered the organic matter composition and deposition in the lagoon. Four phases with varying climates were identified. While autochthonous mangrove C was a significant contributor to carbon accumulation in SAL sediments throughout all four phases, varying admixtures of terrestrial C from the hinterland also contributed, with natural mixed forest C predominating in the early phases and agriculture soil C predominating in the later phases. In this context, climate-related precipitation changes are an overarching control, as surface water transport through rivers serves as the "delivery agent" for the outcomes of the anthropogenic impact in the catchment area into the lagoon. Amongst mangrove-dominated ecosystems globally, the SAL is one of the most effective C sinks due to high mangrove carbon input in combination with a high allochthonous carbon input from anthropogenically enhanced sediment from the hinterland and increased preservation. Given the substantial C sequestration capacity of the SAL and other mangrove-fringed coastal lagoons, conservation and restoration of these ecosystems is vitally important for climate change mitigation.

Identifiants

pubmed: 31820533
doi: 10.1111/gcb.14926
doi:

Substances chimiques

Carbon 7440-44-0

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

1414-1431

Subventions

Organisme : Deutsche Forschungsgemeinschaft
ID : BE-2116/32-1
Pays : International
Organisme : Bundesministerium für Bildung und Forschung
ID : 03F0644A
Pays : International
Organisme : Bundesministerium für Bildung und Forschung
ID : 03F0644B
Pays : International
Organisme : German Academic Exchange Service
Pays : International

Commentaires et corrections

Type : CommentIn

Informations de copyright

© 2019 The Authors. Global Change Biology published by John Wiley & Sons Ltd.

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Auteurs

K Anggi Hapsari (KA)

Department of Palynology and Climate Dynamics, University of Goettingen, Goettingen, Germany.

Tim C Jennerjahn (TC)

Department of Biogeochemistry and Geology, Leibniz Centre for Tropical Marine Research (ZMT), Bremen, Germany.
Faculty of Geosciences, University of Bremen, Bremen, Germany.

Martin C Lukas (MC)

Sustainability Research Center (artec), University of Bremen, MARUM - Center for Marine Environmental Sciences, Bremen, Germany.

Volker Karius (V)

Department of Sedimentology and Environmental Geology, Geoscience Center, University of Goettingen, Goettingen, Germany.

Hermann Behling (H)

Department of Palynology and Climate Dynamics, University of Goettingen, Goettingen, Germany.

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