Strong sesquiterpene emissions from Amazonian soils

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Strong sesquiterpene emissions from Amazonian soils. / Bourtsoukidis, E.; Behrendt, T.; Yañez-Serrano, A. M.; Hellén, H.; Diamantopoulos, E.; Catão, E.; Ashworth, K.; Pozzer, A.; Quesada, C. A.; Martins, D. L.; Sá, M.; Araujo, A.; Brito, J.; Artaxo, P.; Kesselmeier, J.; Lelieveld, J.; Williams, J.

I: Nature Communications, Bind 9, 2226, 2018.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Bourtsoukidis, E, Behrendt, T, Yañez-Serrano, AM, Hellén, H, Diamantopoulos, E, Catão, E, Ashworth, K, Pozzer, A, Quesada, CA, Martins, DL, Sá, M, Araujo, A, Brito, J, Artaxo, P, Kesselmeier, J, Lelieveld, J & Williams, J 2018, 'Strong sesquiterpene emissions from Amazonian soils', Nature Communications, bind 9, 2226. https://doi.org/10.1038/s41467-018-04658-y

APA

Bourtsoukidis, E., Behrendt, T., Yañez-Serrano, A. M., Hellén, H., Diamantopoulos, E., Catão, E., Ashworth, K., Pozzer, A., Quesada, C. A., Martins, D. L., Sá, M., Araujo, A., Brito, J., Artaxo, P., Kesselmeier, J., Lelieveld, J., & Williams, J. (2018). Strong sesquiterpene emissions from Amazonian soils. Nature Communications, 9, [2226]. https://doi.org/10.1038/s41467-018-04658-y

Vancouver

Bourtsoukidis E, Behrendt T, Yañez-Serrano AM, Hellén H, Diamantopoulos E, Catão E o.a. Strong sesquiterpene emissions from Amazonian soils. Nature Communications. 2018;9. 2226. https://doi.org/10.1038/s41467-018-04658-y

Author

Bourtsoukidis, E. ; Behrendt, T. ; Yañez-Serrano, A. M. ; Hellén, H. ; Diamantopoulos, E. ; Catão, E. ; Ashworth, K. ; Pozzer, A. ; Quesada, C. A. ; Martins, D. L. ; Sá, M. ; Araujo, A. ; Brito, J. ; Artaxo, P. ; Kesselmeier, J. ; Lelieveld, J. ; Williams, J. / Strong sesquiterpene emissions from Amazonian soils. I: Nature Communications. 2018 ; Bind 9.

Bibtex

@article{a482a483a2084e71ad57010b71482a8d,
title = "Strong sesquiterpene emissions from Amazonian soils",
abstract = "The Amazon rainforest is the world's largest source of reactive volatile isoprenoids to the atmosphere. It is generally assumed that these emissions are products of photosynthetically driven secondary metabolism and released from the rainforest canopy from where they influence the oxidative capacity of the atmosphere. However, recent measurements indicate that further sources of volatiles are present. Here we show that soil microorganisms are a strong, unaccounted source of highly reactive and previously unreported sesquiterpenes (C15H24; SQT). The emission rate and chemical speciation of soil SQTs were determined as a function of soil moisture, oxygen, and rRNA transcript abundance in the laboratory. Based on these results, a model was developed to predict soil-atmosphere SQT fluxes. It was found SQT emissions from a Terra Firme soil in the dry season were in comparable magnitude to current global model canopy emissions, establishing an important ecological connection between soil microbes and atmospherically relevant SQTs.",
author = "E. Bourtsoukidis and T. Behrendt and Ya{\~n}ez-Serrano, {A. M.} and H. Hell{\'e}n and E. Diamantopoulos and E. Cat{\~a}o and K. Ashworth and A. Pozzer and Quesada, {C. A.} and Martins, {D. L.} and M. S{\'a} and A. Araujo and J. Brito and P. Artaxo and J. Kesselmeier and J. Lelieveld and J. Williams",
year = "2018",
doi = "10.1038/s41467-018-04658-y",
language = "English",
volume = "9",
journal = "Nature Communications",
issn = "2041-1723",
publisher = "nature publishing group",

}

RIS

TY - JOUR

T1 - Strong sesquiterpene emissions from Amazonian soils

AU - Bourtsoukidis, E.

AU - Behrendt, T.

AU - Yañez-Serrano, A. M.

AU - Hellén, H.

AU - Diamantopoulos, E.

AU - Catão, E.

AU - Ashworth, K.

AU - Pozzer, A.

AU - Quesada, C. A.

AU - Martins, D. L.

AU - Sá, M.

AU - Araujo, A.

AU - Brito, J.

AU - Artaxo, P.

AU - Kesselmeier, J.

AU - Lelieveld, J.

AU - Williams, J.

PY - 2018

Y1 - 2018

N2 - The Amazon rainforest is the world's largest source of reactive volatile isoprenoids to the atmosphere. It is generally assumed that these emissions are products of photosynthetically driven secondary metabolism and released from the rainforest canopy from where they influence the oxidative capacity of the atmosphere. However, recent measurements indicate that further sources of volatiles are present. Here we show that soil microorganisms are a strong, unaccounted source of highly reactive and previously unreported sesquiterpenes (C15H24; SQT). The emission rate and chemical speciation of soil SQTs were determined as a function of soil moisture, oxygen, and rRNA transcript abundance in the laboratory. Based on these results, a model was developed to predict soil-atmosphere SQT fluxes. It was found SQT emissions from a Terra Firme soil in the dry season were in comparable magnitude to current global model canopy emissions, establishing an important ecological connection between soil microbes and atmospherically relevant SQTs.

AB - The Amazon rainforest is the world's largest source of reactive volatile isoprenoids to the atmosphere. It is generally assumed that these emissions are products of photosynthetically driven secondary metabolism and released from the rainforest canopy from where they influence the oxidative capacity of the atmosphere. However, recent measurements indicate that further sources of volatiles are present. Here we show that soil microorganisms are a strong, unaccounted source of highly reactive and previously unreported sesquiterpenes (C15H24; SQT). The emission rate and chemical speciation of soil SQTs were determined as a function of soil moisture, oxygen, and rRNA transcript abundance in the laboratory. Based on these results, a model was developed to predict soil-atmosphere SQT fluxes. It was found SQT emissions from a Terra Firme soil in the dry season were in comparable magnitude to current global model canopy emissions, establishing an important ecological connection between soil microbes and atmospherically relevant SQTs.

UR - http://www.scopus.com/inward/record.url?scp=85048264277&partnerID=8YFLogxK

U2 - 10.1038/s41467-018-04658-y

DO - 10.1038/s41467-018-04658-y

M3 - Journal article

C2 - 29884892

AN - SCOPUS:85048264277

VL - 9

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

M1 - 2226

ER -

ID: 198722363