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dc.contributor.authorStötter, Tabea
dc.contributor.authorBastviken, David
dc.contributor.authorBodelier, Paul L.E.
dc.contributor.authorvan Hardenbroek, Maarten
dc.contributor.authorRinta, Päivi
dc.contributor.authorSchilder, Johannes
dc.contributor.authorSchubert, Carsten J.
dc.contributor.authorHeiri, Oliver
dc.date.accessioned2019-01-14T10:22:02Z
dc.date.available2020-07-01T21:35:08Z
dc.date.issued2018
dc.identifier.citationStötter, T., Bastviken, D., Bodelier, P. L., van Hardenbroek, M., Rinta, P., Schilder, J., Schubert, C. J., & Heiri, O. (2018). Abundance and δ13C values of fatty acids in lacustrine surface sediments : Relationships with in-lake methane concentrations. <i>Quaternary Science Reviews</i>, <i>191</i>, 337-347. <a href="https://doi.org/10.1016/j.quascirev.2018.04.029" target="_blank">https://doi.org/10.1016/j.quascirev.2018.04.029</a>
dc.identifier.otherCONVID_28071488
dc.identifier.otherTUTKAID_77737
dc.identifier.urihttps://jyx.jyu.fi/handle/123456789/62454
dc.description.abstractProxy-indicators in lake sediments provide the only approach by which the dynamics of in-lake methane cycling can be examined on multi-decadal to centennial time scales. This information is necessary to constrain how lacustrine methane production, oxidation and emissions are expected to respond to global change drivers. Several of the available proxies for reconstructing methane cycle changes of lakes rely on interpreting past changes in the abundance or relevance of methane oxidizing bacteria (MOB), either directly (e.g. via analysis of bacterial lipids) or indirectly (e.g. via reconstructions of the past relevance of MOB in invertebrate diet). However, only limited information is available about the extent to which, at the ecosystem scale, variations in abundance and availability of MOB reflect past changes in in-lake methane concentrations. We present a study examining the abundances of fatty acids (FAs), particularly of 13C-depleted FAs known to be produced by MOB, relative to methane concentrations in 29 small European lakes. 39 surface sediment samples were obtained from these lakes and FA abundances were compared with methane concentrations measured at the lake surface, 10 cm above the sediments and 10 cm within the sediments. Three of the FAs in the surface sediment samples, C16:1ω7c, C16:1ω5c/t, and C18:1ω7c were characterized by lower δ13C values than the remaining FAs. We show that abundances of these FAs, relative to other short-chain FAs produced in lake ecosystems, are related with sedimentary MOB concentrations assessed by quantitative polymerase chain reaction (qPCR). We observed positive relationships between methane concentrations and relative abundances of C16:1ω7c, C16:1ω5c/t, and C18:1ω7c and the sum of these FAs. For the full dataset these relationships were relatively weak (Spearman's rank correlation (rs) of 0.34–0.43) and not significant if corrected for multiple testing. However, noticeably stronger and statistically significant relationships were observed when sediments from near-shore and deep-water oxic environments (rs = 0.57 to 0.62) and those from anoxic deep-water environment (rs = 0.55 to 0.65) were examined separately. Our results confirm that robust relationships exist between in-lake CH4 concentrations and 13C-depleted groups of FAs in the examined sediments, agreeing with earlier suggestions that the availability of MOB-derived, 13C-depleted organic matter for aquatic invertebrates increases with increasing methane concentrations. However, we also show that these relationships are complex, with different relationships observed for oxic and anoxic sediments and highest values measured in sediments deposited in oxic environments overlain with relatively methane-rich water. Furthermore, although all three 13C-depleted FA groups identified in our survey are known to be produced by MOB, they also receive contributions by other organism groups, and this will have influenced their distribution in our dataset.fi
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherPergamon Press
dc.relation.ispartofseriesQuaternary Science Reviews
dc.rightsCC BY-NC-ND 4.0
dc.subject.othermethane oxidizing bacteria
dc.subject.otherstable carbon isotopes
dc.subject.otheraquatic invertebrates
dc.subject.othersediment
dc.titleAbundance and δ13C values of fatty acids in lacustrine surface sediments : Relationships with in-lake methane concentrations
dc.typearticle
dc.identifier.urnURN:NBN:fi:jyu-201901091131
dc.contributor.laitosBio- ja ympäristötieteiden laitosfi
dc.contributor.laitosDepartment of Biological and Environmental Scienceen
dc.contributor.oppiaineAkvaattiset tieteetfi
dc.contributor.oppiaineAquatic Sciencesen
dc.type.urihttp://purl.org/eprint/type/JournalArticle
dc.date.updated2019-01-09T10:15:13Z
dc.description.reviewstatuspeerReviewed
dc.format.pagerange337-347
dc.relation.issn0277-3791
dc.relation.numberinseries0
dc.relation.volume191
dc.type.versionacceptedVersion
dc.rights.copyright© 2018 Elsevier Ltd.
dc.rights.accesslevelopenAccessfi
dc.subject.ysometaani
dc.subject.ysorasvahapot
dc.subject.ysoisotoopit
dc.subject.ysoselkärangattomat
dc.subject.ysojärvet
dc.subject.ysosedimentit
dc.format.contentfulltext
jyx.subject.urihttp://www.yso.fi/onto/yso/p13222
jyx.subject.urihttp://www.yso.fi/onto/yso/p4800
jyx.subject.urihttp://www.yso.fi/onto/yso/p6387
jyx.subject.urihttp://www.yso.fi/onto/yso/p3931
jyx.subject.urihttp://www.yso.fi/onto/yso/p9374
jyx.subject.urihttp://www.yso.fi/onto/yso/p14605
dc.rights.urlhttps://creativecommons.org/licenses/by-nc-nd/4.0/
dc.relation.doi10.1016/j.quascirev.2018.04.029


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