Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?

Tropical peatlands hold large amounts of carbon but the influence of litter inputs and variation in peat properties with depth on carbon storage are poorly understood. Here we present a stratigraphy of peatland carbon stocks and accumulation through the peat profile in a tropical ombrotrophic wetlan...

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Main Authors: Upton, Abbie, Vane, Christopher H., Girkin, Nick, Turner, Benjamin L., Sjögersten, Sofie
Format: Article
Published: Elsevier 2018
Subjects:
Online Access:https://eprints.nottingham.ac.uk/52567/
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author Upton, Abbie
Vane, Christopher H.
Girkin, Nick
Turner, Benjamin L.
Sjögersten, Sofie
author_facet Upton, Abbie
Vane, Christopher H.
Girkin, Nick
Turner, Benjamin L.
Sjögersten, Sofie
author_sort Upton, Abbie
building Nottingham Research Data Repository
collection Online Access
description Tropical peatlands hold large amounts of carbon but the influence of litter inputs and variation in peat properties with depth on carbon storage are poorly understood. Here we present a stratigraphy of peatland carbon stocks and accumulation through the peat profile in a tropical ombrotrophic wetland and assess shifts in vegetation inputs and organic matter degradation using n-alkane distributions and Rock-Eval 6 pyrolysis. Mixed forest (including canopy palms and tropical hardwood trees) contained the greatest total carbon stock in the soil (1884 Mg C ha−1), followed by Rhizophora mangle (mangrove, 1771 Mg C ha−1), Campnosperma panamensis (hardwood, 1694 Mg C ha−1) and Cyperus (sawgrass) bog plain (1488 Mg C ha−1). The long-term apparent rate of carbon accumulation, determined by 14C dating of the carbon stored in different layers in the peat profile, decreased from the edge to the interior of the peatland, with the highest accumulation rate in at the Rhizophora site (102.2 g C m−2 y−1) and the lowest in the deeper peat layers at the Cyperus site (45.6 g C m−2 y−1). High molecular weight n-alkanes dominated in surface peat in all four phasic communities, while deeper in the peat profile n-alkane profiles differed more among sites, suggesting contrasting litter inputs or decomposition environments. Deeper peat was depleted in carbohydrates and had a relatively larger thermostable C pool. Taken together our findings show (i) that different forest types hold varying C stocks and have different peat accumulation rates, even over relatively small distances, and (ii) progressive depletion of carbohydrates and thermolabile compounds with depth, despite strong variation in litter inputs throughout the peat profile.
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spelling nottingham-525672020-05-04T19:49:13Z https://eprints.nottingham.ac.uk/52567/ Does litter input determine carbon storage and peat organic chemistry in tropical peatlands? Upton, Abbie Vane, Christopher H. Girkin, Nick Turner, Benjamin L. Sjögersten, Sofie Tropical peatlands hold large amounts of carbon but the influence of litter inputs and variation in peat properties with depth on carbon storage are poorly understood. Here we present a stratigraphy of peatland carbon stocks and accumulation through the peat profile in a tropical ombrotrophic wetland and assess shifts in vegetation inputs and organic matter degradation using n-alkane distributions and Rock-Eval 6 pyrolysis. Mixed forest (including canopy palms and tropical hardwood trees) contained the greatest total carbon stock in the soil (1884 Mg C ha−1), followed by Rhizophora mangle (mangrove, 1771 Mg C ha−1), Campnosperma panamensis (hardwood, 1694 Mg C ha−1) and Cyperus (sawgrass) bog plain (1488 Mg C ha−1). The long-term apparent rate of carbon accumulation, determined by 14C dating of the carbon stored in different layers in the peat profile, decreased from the edge to the interior of the peatland, with the highest accumulation rate in at the Rhizophora site (102.2 g C m−2 y−1) and the lowest in the deeper peat layers at the Cyperus site (45.6 g C m−2 y−1). High molecular weight n-alkanes dominated in surface peat in all four phasic communities, while deeper in the peat profile n-alkane profiles differed more among sites, suggesting contrasting litter inputs or decomposition environments. Deeper peat was depleted in carbohydrates and had a relatively larger thermostable C pool. Taken together our findings show (i) that different forest types hold varying C stocks and have different peat accumulation rates, even over relatively small distances, and (ii) progressive depletion of carbohydrates and thermolabile compounds with depth, despite strong variation in litter inputs throughout the peat profile. Elsevier 2018-09-15 Article PeerReviewed Upton, Abbie, Vane, Christopher H., Girkin, Nick, Turner, Benjamin L. and Sjögersten, Sofie (2018) Does litter input determine carbon storage and peat organic chemistry in tropical peatlands? Geoderma, 326 . pp. 76-87. ISSN 0016-7061 Carbon storage ; Decomposition ; Tropical peatland ; Rock-Eval pyrolysis ; n-Alkanes ; FTIR https://www.sciencedirect.com/science/article/pii/S0016706117320128 doi:10.1016/j.geoderma.2018.03.030 doi:10.1016/j.geoderma.2018.03.030
spellingShingle Carbon storage ; Decomposition ; Tropical peatland ; Rock-Eval pyrolysis ; n-Alkanes ; FTIR
Upton, Abbie
Vane, Christopher H.
Girkin, Nick
Turner, Benjamin L.
Sjögersten, Sofie
Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
title Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
title_full Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
title_fullStr Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
title_full_unstemmed Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
title_short Does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
title_sort does litter input determine carbon storage and peat organic chemistry in tropical peatlands?
topic Carbon storage ; Decomposition ; Tropical peatland ; Rock-Eval pyrolysis ; n-Alkanes ; FTIR
url https://eprints.nottingham.ac.uk/52567/
https://eprints.nottingham.ac.uk/52567/
https://eprints.nottingham.ac.uk/52567/