Poeplau C - Search Results

1

The legacy of one hundred years of climate change for organic carbon stocks in global agricultural topsoils.

Poeplau C, Dechow R. Poeplau C, et al. Sci Rep. 2023 May 9;13(1):7483. doi: 10.1038/s41598-023-34753-0. Sci Rep. 2023. PMID: 37160983 Free PMC article.

2

Projected loss of soil organic carbon in temperate agricultural soils in the 21(st) century: effects of climate change and carbon input trends.

Wiesmeier M, Poeplau C, Sierra CA, Maier H, Frühauf C, Hübner R, Kühnel A, Spörlein P, Geuß U, Hangen E, Schilling B, von Lützow M, Kögel-Knabner I. Wiesmeier M, et al. Among authors: poeplau c. Sci Rep. 2016 Sep 2;6:32525. doi: 10.1038/srep32525. Sci Rep. 2016. PMID: 27585648 Free PMC article.

3

Root litter quality drives the dynamic of native mineral-associated organic carbon in a temperate agricultural soil.

Poeplau C, Begill N, Liang Z, Schiedung M. Poeplau C, et al. Plant Soil. 2023;491(1-2):439-456. doi: 10.1007/s11104-023-06127-y. Epub 2023 Jun 21. Plant Soil. 2023. PMID: 37869369 Free PMC article.

4

Impact of land-use change and soil organic carbon quality on microbial diversity in soils across Europe.

Szoboszlay M, Dohrmann AB, Poeplau C, Don A, Tebbe CC. Szoboszlay M, et al. Among authors: poeplau c. FEMS Microbiol Ecol. 2017 Dec 1;93(12). doi: 10.1093/femsec/fix146. FEMS Microbiol Ecol. 2017. PMID: 29087486

5

Long-term geothermal warming reduced stocks of carbon but not nitrogen in a subarctic forest soil.

Peplau T, Schroeder J, Gregorich E, Poeplau C. Peplau T, et al. Among authors: poeplau c. Glob Chang Biol. 2021 Oct;27(20):5341-5355. doi: 10.1111/gcb.15754. Epub 2021 Jul 10. Glob Chang Biol. 2021. PMID: 34157198

6

Roots are key to increasing the mean residence time of organic carbon entering temperate agricultural soils.

Poeplau C, Don A, Schneider F. Poeplau C, et al. Glob Chang Biol. 2021 Oct;27(19):4921-4934. doi: 10.1111/gcb.15787. Epub 2021 Jul 18. Glob Chang Biol. 2021. PMID: 34228862

7

Subarctic soil carbon losses after deforestation for agriculture depend on permafrost abundance.

Peplau T, Schroeder J, Gregorich E, Poeplau C. Peplau T, et al. Among authors: poeplau c. Glob Chang Biol. 2022 Sep;28(17):5227-5242. doi: 10.1111/gcb.16307. Epub 2022 Jul 5. Glob Chang Biol. 2022. PMID: 35713970

8

No detectable upper limit of mineral-associated organic carbon in temperate agricultural soils.

Begill N, Don A, Poeplau C. Begill N, et al. Among authors: poeplau c. Glob Chang Biol. 2023 Aug;29(16):4662-4669. doi: 10.1111/gcb.16804. Epub 2023 Jun 4. Glob Chang Biol. 2023. PMID: 37271832

9

Sensitivity of soil carbon fractions and their specific stabilization mechanisms to extreme soil warming in a subarctic grassland.

Poeplau C, Kätterer T, Leblans NI, Sigurdsson BD. Poeplau C, et al. Glob Chang Biol. 2017 Mar;23(3):1316-1327. doi: 10.1111/gcb.13491. Epub 2016 Sep 19. Glob Chang Biol. 2017. PMID: 27591579

10

Predicting ecosystem responses by data-driven reciprocal modelling.

Schneider F, Poeplau C, Don A. Schneider F, et al. Among authors: poeplau c. Glob Chang Biol. 2021 Nov;27(21):5670-5679. doi: 10.1111/gcb.15817. Epub 2021 Aug 14. Glob Chang Biol. 2021. PMID: 34351036

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