Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance
Large peatlands exist at high latitudes because flooded conditions and cold temperatures slow decomposition, so the presence of (sub)tropical peat is enigmatic. Here the authors show that low-latitude peat is preserved due to lower carbohydrate and greater aromatic content resulting in chemical reca...
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Nature Portfolio
2018
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oai:doaj.org-article:b84cbfe663344ab68ee193f1479d2bbf2021-12-02T16:56:58ZTropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance10.1038/s41467-018-06050-22041-1723https://doaj.org/article/b84cbfe663344ab68ee193f1479d2bbf2018-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-06050-2https://doaj.org/toc/2041-1723Large peatlands exist at high latitudes because flooded conditions and cold temperatures slow decomposition, so the presence of (sub)tropical peat is enigmatic. Here the authors show that low-latitude peat is preserved due to lower carbohydrate and greater aromatic content resulting in chemical recalcitrance.Suzanne B. HodgkinsCurtis J. RichardsonRené DommainHongjun WangPaul H. GlaserBrittany VerbekeB. Rose WinklerAlexander R. CobbVirginia I. RichMalak MissilmaniNeal FlanaganMengchi HoAlison M. HoytCharles F. HarveyS. Rose ViningMoira A. HoughTim R. MoorePierre J. H. RichardFlorentino B. De La CruzJoumana ToufailyRasha HamdanWilliam T. CooperJeffrey P. ChantonNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-13 (2018) |
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Science Q Suzanne B. Hodgkins Curtis J. Richardson René Dommain Hongjun Wang Paul H. Glaser Brittany Verbeke B. Rose Winkler Alexander R. Cobb Virginia I. Rich Malak Missilmani Neal Flanagan Mengchi Ho Alison M. Hoyt Charles F. Harvey S. Rose Vining Moira A. Hough Tim R. Moore Pierre J. H. Richard Florentino B. De La Cruz Joumana Toufaily Rasha Hamdan William T. Cooper Jeffrey P. Chanton Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
description |
Large peatlands exist at high latitudes because flooded conditions and cold temperatures slow decomposition, so the presence of (sub)tropical peat is enigmatic. Here the authors show that low-latitude peat is preserved due to lower carbohydrate and greater aromatic content resulting in chemical recalcitrance. |
format |
article |
author |
Suzanne B. Hodgkins Curtis J. Richardson René Dommain Hongjun Wang Paul H. Glaser Brittany Verbeke B. Rose Winkler Alexander R. Cobb Virginia I. Rich Malak Missilmani Neal Flanagan Mengchi Ho Alison M. Hoyt Charles F. Harvey S. Rose Vining Moira A. Hough Tim R. Moore Pierre J. H. Richard Florentino B. De La Cruz Joumana Toufaily Rasha Hamdan William T. Cooper Jeffrey P. Chanton |
author_facet |
Suzanne B. Hodgkins Curtis J. Richardson René Dommain Hongjun Wang Paul H. Glaser Brittany Verbeke B. Rose Winkler Alexander R. Cobb Virginia I. Rich Malak Missilmani Neal Flanagan Mengchi Ho Alison M. Hoyt Charles F. Harvey S. Rose Vining Moira A. Hough Tim R. Moore Pierre J. H. Richard Florentino B. De La Cruz Joumana Toufaily Rasha Hamdan William T. Cooper Jeffrey P. Chanton |
author_sort |
Suzanne B. Hodgkins |
title |
Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
title_short |
Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
title_full |
Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
title_fullStr |
Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
title_full_unstemmed |
Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
title_sort |
tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance |
publisher |
Nature Portfolio |
publishDate |
2018 |
url |
https://doaj.org/article/b84cbfe663344ab68ee193f1479d2bbf |
work_keys_str_mv |
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