Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows

This study evaluated the effects of biogenic structures (tree roots and crab burrows) on sediment carbon (C), sulfur (S), and iron (Fe) biogeochemistry during the wet season in the Olaria mangrove forests near the city of Cananéia, São Paulo state, Brazil and the Nobrega mangrove forest approximate...

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Main Authors: Erik Kristensen, Thomas Valdemarsen, Paula C. de Moraes, Arthur Z. Güth, Paulo Y. G. Sumida, Cintia O. Quintana
Format: Article
Language:English
Published: Instituto Oceanográfico da Universidade de São Paulo 2022-12-01
Series:Ocean and Coastal Research
Subjects:
Online Access:https://journals.usp.br/ocr/article/view/205208
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author Erik Kristensen
Thomas Valdemarsen
Paula C. de Moraes
Arthur Z. Güth
Paulo Y. G. Sumida
Cintia O. Quintana
author_facet Erik Kristensen
Thomas Valdemarsen
Paula C. de Moraes
Arthur Z. Güth
Paulo Y. G. Sumida
Cintia O. Quintana
author_sort Erik Kristensen
collection DOAJ
description This study evaluated the effects of biogenic structures (tree roots and crab burrows) on sediment carbon (C), sulfur (S), and iron (Fe) biogeochemistry during the wet season in the Olaria mangrove forests near the city of Cananéia, São Paulo state, Brazil and the Nobrega mangrove forest approximately 2 km from the city. Anaerobic C oxidation pathways were assessed from sediment profiles and anaerobic incubations and related to the abundance of biogenic structures in the form of pneumatophores and crab burrows. Porewater depth profiles of dissolved inorganic carbon (DIC) and SO42- were less steep in the presence than absence of biogenic structures. While Fe(II) appeared unaffected by biogenic structures, Fe(III) levels were significantly higher in the upper 4 cm of the sediment in the presence than absence of vegetation and bioturbation. Surprisingly, the concentration of Fe(III) in this layer was 2-6 times higher in the Nobrega forest (6-13 µmol cm-3) than in the Olaria forest (1.5-6.5 µmol cm-3). Accordingly, depth integrated sulfate reduction (SR) tended to be highest at Olaria, while iron reduction (FeR) was highest at Nobrega. SR accounted for 54-83% of DIC production, with no diference between forested sites, while FeR accounted for 8-24% of DIC production, with a 2-3 times higher contribution in the Nobrega versus the Olaria forest. The results suggest that mangrove roots and crab burrows in mangrove sediments only promote FeR at the expense of SR in the Nobrega forest. It appears that anthropogenic discharge from Cananéia city may have overridden the impact of biogenic structures on sediment redox conditions at Olaria, thereby diminishing the role of FeR without strong stimulation of overall C oxidation rates.
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spelling doaj-art-fe7b7f16dc0644c79ec681ff102367d92025-08-20T03:19:11ZengInstituto Oceanográfico da Universidade de São PauloOcean and Coastal Research2675-28242022-12-0171Suppl. 1Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrowsErik KristensenThomas ValdemarsenPaula C. de MoraesArthur Z. GüthPaulo Y. G. SumidaCintia O. Quintana This study evaluated the effects of biogenic structures (tree roots and crab burrows) on sediment carbon (C), sulfur (S), and iron (Fe) biogeochemistry during the wet season in the Olaria mangrove forests near the city of Cananéia, São Paulo state, Brazil and the Nobrega mangrove forest approximately 2 km from the city. Anaerobic C oxidation pathways were assessed from sediment profiles and anaerobic incubations and related to the abundance of biogenic structures in the form of pneumatophores and crab burrows. Porewater depth profiles of dissolved inorganic carbon (DIC) and SO42- were less steep in the presence than absence of biogenic structures. While Fe(II) appeared unaffected by biogenic structures, Fe(III) levels were significantly higher in the upper 4 cm of the sediment in the presence than absence of vegetation and bioturbation. Surprisingly, the concentration of Fe(III) in this layer was 2-6 times higher in the Nobrega forest (6-13 µmol cm-3) than in the Olaria forest (1.5-6.5 µmol cm-3). Accordingly, depth integrated sulfate reduction (SR) tended to be highest at Olaria, while iron reduction (FeR) was highest at Nobrega. SR accounted for 54-83% of DIC production, with no diference between forested sites, while FeR accounted for 8-24% of DIC production, with a 2-3 times higher contribution in the Nobrega versus the Olaria forest. The results suggest that mangrove roots and crab burrows in mangrove sediments only promote FeR at the expense of SR in the Nobrega forest. It appears that anthropogenic discharge from Cananéia city may have overridden the impact of biogenic structures on sediment redox conditions at Olaria, thereby diminishing the role of FeR without strong stimulation of overall C oxidation rates. https://journals.usp.br/ocr/article/view/205208Sulfate reductionIron reductionBiogeochemistryMangrove rootsCrab burrows
spellingShingle Erik Kristensen
Thomas Valdemarsen
Paula C. de Moraes
Arthur Z. Güth
Paulo Y. G. Sumida
Cintia O. Quintana
Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows
Ocean and Coastal Research
Sulfate reduction
Iron reduction
Biogeochemistry
Mangrove roots
Crab burrows
title Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows
title_full Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows
title_fullStr Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows
title_full_unstemmed Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows
title_short Anaerobic carbon oxidation in sediment of two Brazilian mangrove forests: the influence of tree roots and crab burrows
title_sort anaerobic carbon oxidation in sediment of two brazilian mangrove forests the influence of tree roots and crab burrows
topic Sulfate reduction
Iron reduction
Biogeochemistry
Mangrove roots
Crab burrows
url https://journals.usp.br/ocr/article/view/205208
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