ArticleNature communications2026
Catchment lithology controls net carbon balance along the Antarctic Peninsula.
Songfan He, Xiaowen Zhang, Huanting Hu, Maojun Yan, Huiyuan Yang, Qiyue Gu, Thomas S Bianchi, Xiaomei Xu, Xingqian Cui
Abstract read
In one paragraphArticle in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
0numbers the graph read from it
0cells of the map it votes in
0citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from itWhat it found
Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.
The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
2 · The registryThe trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.
3 · Its place in the literatureWho cites it
0 citing papers in PubMed.
No citing paper in PubMed yet.
4 · The recordCorrections and comments
PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.
5 · Who and what moneyAuthors and funding
9 authors.
Songfan HeState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.ORCID http://orcid.org/0009-0000-7518-8245 Xiaowen ZhangState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China. xiaowenz@sjtu.edu.cn.ORCID http://orcid.org/0000-0001-8768-1459 Huanting HuState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.
Maojun YanState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.
Huiyuan YangState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.
Qiyue GuState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China.
Thomas S BianchiInstitute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH, USA.
Xingqian CuiState Key Laboratory of Submarine Geoscience; Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai, China. cuixingqian@sjtu.edu.cn.ORCID http://orcid.org/0000-0001-6705-7595 Funding
National Natural Science Foundation of China (National Science Foundation of China) 42206034National Natural Science Foundation of China (National Science Foundation of China) 42273075Shanghai Science and Technology Development Foundation (Shanghai Science and Technology Development Fund) 24QA2704000
6 · The paper itselfAbstract
Climate-driven ecosystem change in Antarctica is reshaping carbon dynamics and influencing global climate. Under sustained warming, mobilization and reburial of organic carbon (OC) in coastal Antarctica may represent an important carbon sink, yet regional OC burial and oxidation remain poorly quantified. Here, we apply ramped pyrolysis/oxidation analysis and isotopic end-member mixing models to investigate sedimentary OC along two Western Antarctic Peninsula (WAP) fjords underlain by contrasting bedrock types. We show that the fjord underlain by sedimentary rocks exhibits ten-fold higher burial flux of petrogenic OC (OC
Identifiers
PMID42303987
PMCPMC13434350
What OpenQuestion holds
Textmetadata
LicenceCC BY-NC-ND
Read underepoch 390