The role of reactive iron in long-term carbon sequestration in mangrove sediments
Despite occupying only 0.5% of the global coastal ocean, mangroves play a disproportionately large role in the capture and retention of atmospheric carbon dioxide as organic carbon (OC) in its sediments. However, the capacity of mangrove sediments to store high amounts of OC has never been explained mechanistically. This study elucidates the role of reactive iron (FeR) in long-term carbon sequestration in mangrove sediments.
Materials and methods
Sediment samples of up to 1 m in depth were collected from six selected mangrove areas across the Philippines. The samples were characterized using X-ray diffraction (XRD) and X-ray fluorescence (XRF). A citrate-bicarbonate-dithionite reduction procedure was employed to extract FeR from the sediments. The OC concentration and δ13C signatures before and after FeR extraction were determined using a dichromate oxidation technique and isotope ratio mass spectrometry (IRMS), respectively.
Results and discussion
XRD diffractograms showed that the mangrove sediment samples varied in terms of mineralogical characteristics, which reflected their different parent materials. It was found that the OC concentration increased exponentially (OC = 8.38e0.37FeR; R2 = 0.88; p < 0.0001) with increasing FeR concentration. δ13C signatures of FeR-associated OC revealed that FeR preferentially preserved terrestrial over marine-derived organic matter. Finally, FeR was estimated to coprecipitate with up to 5.44 × 1012 g OC in mangrove sediments per year.
The findings of this study suggest that FeR is responsible for the preservation of OC, thus making mangrove sediments a “giant rusty sponge” for carbon. This mechanistic understanding of the long-term carbon storage in mangrove sediments could help draft better strategies for blue carbon initiatives that include the mangrove ecosystems.
KeywordsCarbon sequestration Mangrove sediments Organic matter preservation Reactive iron Stable isotope
This study was supported by the Department of Science and Technology Accelerated Science and Technology Human Resource Development Program—National Science Consortium (DOST ASTHRDP-NSC); the Philippine Nuclear Research Institute Graduate Student Research Grant Program (PNRI GSRGP), with funding from the Philippine Council for Industry, Energy and Emerging Technologies (PCIEERD); and the United States Agency for International Development (USAID) through the Partnership for Enhanced Engagement in Research (PEER) of the National Science Foundation (NSF; Project 3-191). The University Research Council of Ateneo de Manila University has granted a research faculty fellowship to Ian A. Navarrete during the preparation of the manuscript.
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