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Soil carbon storage is related to tree functional composition in naturally regenerating tropical forests

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Soil carbon storage is related to tree functional composition in naturally regenerating tropical forests. / Wallwork, Abby; Banin, Lindsay F.; Dent, Daisy H. et al.
In: Functional Ecology, Vol. 36, No. 12, 31.12.2022, p. 3175-3187.

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Wallwork A, Banin LF, Dent DH, Skiba U, Sayer E. Soil carbon storage is related to tree functional composition in naturally regenerating tropical forests. Functional Ecology. 2022 Dec 31;36(12):3175-3187. Epub 2022 Nov 10. doi: 10.1111/1365-2435.14221

Author

Wallwork, Abby ; Banin, Lindsay F. ; Dent, Daisy H. et al. / Soil carbon storage is related to tree functional composition in naturally regenerating tropical forests. In: Functional Ecology. 2022 ; Vol. 36, No. 12. pp. 3175-3187.

Bibtex

@article{88a3d020251f4d5995af523bf9c4374c,
title = "Soil carbon storage is related to tree functional composition in naturally regenerating tropical forests",
abstract = "1. Regenerating tropical forests are increasingly important for their role in the global carbon cycle. Carbon stocks in aboveground biomass can recover to old-growth forest levels within 60-100 years. However more than half of all carbon in tropical forests is stored belowground, and our understanding of carbon storage in soils during tropical forest recovery is limited.2. Importantly, soil carbon accumulation does not necessarily reflect patterns in aboveground biomass carbon accrual during secondary forest succession and factors related to past land-use, species composition, and soil characteristics may influence soil carbon storage during forest regrowth.3. Using tree census data and a measure of tree community shade tolerance (species-specific light response values), we assessed the relationship between soil organic carbon stocks and tree functional groups during secondary succession along a chronosequence of 40–120-year-old naturally regenerating secondary forest and old-growth tropical forest stands in Panama.4. Whereas previous studies found no evidence for increasing soil C storage with secondary forest age, we found a strong relationship between tree functional composition and soil carbon stocks at 0-10 cm depth, whereby carbon stocks increased with the relative influence of light-demanding tree species. Light demanding trees had higher leaf nitrogen but lower leaf density than shade-tolerant trees, suggesting that rapid decomposition of nutrient-rich plant material in forests with a higher proportion of light-demanding species results in greater accumulation of carbon in the surface layer of soils.5. Synthesis. We propose that soil carbon storage in secondary tropical forests is more strongly linked to tree functional composition than forest age, and that the persistence of long-lived pioneer trees could enhance soil carbon storage as forests age. Considering shifts in tree functional groups could improve estimates of carbon sequestration potential for climate change mitigation by tropical forest regrowth.",
keywords = "Ecology, Evolution, Behavior and Systematics",
author = "Abby Wallwork and Banin, {Lindsay F.} and Dent, {Daisy H.} and Ute Skiba and Emma Sayer",
year = "2022",
month = dec,
day = "31",
doi = "10.1111/1365-2435.14221",
language = "English",
volume = "36",
pages = "3175--3187",
journal = "Functional Ecology",
issn = "0269-8463",
publisher = "Blackwell Publishing Ltd",
number = "12",

}

RIS

TY - JOUR

T1 - Soil carbon storage is related to tree functional composition in naturally regenerating tropical forests

AU - Wallwork, Abby

AU - Banin, Lindsay F.

AU - Dent, Daisy H.

AU - Skiba, Ute

AU - Sayer, Emma

PY - 2022/12/31

Y1 - 2022/12/31

N2 - 1. Regenerating tropical forests are increasingly important for their role in the global carbon cycle. Carbon stocks in aboveground biomass can recover to old-growth forest levels within 60-100 years. However more than half of all carbon in tropical forests is stored belowground, and our understanding of carbon storage in soils during tropical forest recovery is limited.2. Importantly, soil carbon accumulation does not necessarily reflect patterns in aboveground biomass carbon accrual during secondary forest succession and factors related to past land-use, species composition, and soil characteristics may influence soil carbon storage during forest regrowth.3. Using tree census data and a measure of tree community shade tolerance (species-specific light response values), we assessed the relationship between soil organic carbon stocks and tree functional groups during secondary succession along a chronosequence of 40–120-year-old naturally regenerating secondary forest and old-growth tropical forest stands in Panama.4. Whereas previous studies found no evidence for increasing soil C storage with secondary forest age, we found a strong relationship between tree functional composition and soil carbon stocks at 0-10 cm depth, whereby carbon stocks increased with the relative influence of light-demanding tree species. Light demanding trees had higher leaf nitrogen but lower leaf density than shade-tolerant trees, suggesting that rapid decomposition of nutrient-rich plant material in forests with a higher proportion of light-demanding species results in greater accumulation of carbon in the surface layer of soils.5. Synthesis. We propose that soil carbon storage in secondary tropical forests is more strongly linked to tree functional composition than forest age, and that the persistence of long-lived pioneer trees could enhance soil carbon storage as forests age. Considering shifts in tree functional groups could improve estimates of carbon sequestration potential for climate change mitigation by tropical forest regrowth.

AB - 1. Regenerating tropical forests are increasingly important for their role in the global carbon cycle. Carbon stocks in aboveground biomass can recover to old-growth forest levels within 60-100 years. However more than half of all carbon in tropical forests is stored belowground, and our understanding of carbon storage in soils during tropical forest recovery is limited.2. Importantly, soil carbon accumulation does not necessarily reflect patterns in aboveground biomass carbon accrual during secondary forest succession and factors related to past land-use, species composition, and soil characteristics may influence soil carbon storage during forest regrowth.3. Using tree census data and a measure of tree community shade tolerance (species-specific light response values), we assessed the relationship between soil organic carbon stocks and tree functional groups during secondary succession along a chronosequence of 40–120-year-old naturally regenerating secondary forest and old-growth tropical forest stands in Panama.4. Whereas previous studies found no evidence for increasing soil C storage with secondary forest age, we found a strong relationship between tree functional composition and soil carbon stocks at 0-10 cm depth, whereby carbon stocks increased with the relative influence of light-demanding tree species. Light demanding trees had higher leaf nitrogen but lower leaf density than shade-tolerant trees, suggesting that rapid decomposition of nutrient-rich plant material in forests with a higher proportion of light-demanding species results in greater accumulation of carbon in the surface layer of soils.5. Synthesis. We propose that soil carbon storage in secondary tropical forests is more strongly linked to tree functional composition than forest age, and that the persistence of long-lived pioneer trees could enhance soil carbon storage as forests age. Considering shifts in tree functional groups could improve estimates of carbon sequestration potential for climate change mitigation by tropical forest regrowth.

KW - Ecology, Evolution, Behavior and Systematics

U2 - 10.1111/1365-2435.14221

DO - 10.1111/1365-2435.14221

M3 - Journal article

VL - 36

SP - 3175

EP - 3187

JO - Functional Ecology

JF - Functional Ecology

SN - 0269-8463

IS - 12

ER -