ADEARTH

Advances in Earth Science >

2014 , Vol. 29 >Issue 11: 1294 - 1297

DOI: https://doi.org/10.11867/j.issn.1001-8166.2014.11.1294

Orginal Article

To Decipher the Ocean Carbon Sink Through Interdisciplinarity and the Integration of the Past and Present

  • Nianzhi Jiao ,
  • Chuanlun Zhang ,
  • Shucheng Xie ,
  • Jihua Liu ,
  • Fei Zhang
Expand
  • 1. State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361102, China
    2. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China; .State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan430074, China
    3. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan430074, China

Online published: 2014-11-20

Copyright

地球科学进展 编辑部, 2014, This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Fold

Abstract

The ocean is the world’s largest active carbon pool and buffers global climate change. Current scientific research focuses on ocean carbon cycling and carbon sequestration mechanisms. The new cognition can be successfully reached only through interdisciplinary and integrative studies of the past and present oceans.

Key words： Ocean carbon sink; Carbon cycling; Microbial Carbon Pump; Archaea; Paleoenvironments.

Cite this article

Nianzhi Jiao , Chuanlun Zhang , Shucheng Xie , Jihua Liu , Fei Zhang . To Decipher the Ocean Carbon Sink Through Interdisciplinarity and the Integration of the Past and Present[J]. Advances in Earth Science, 2014 , 29(11) : 1294 -1297 . DOI: 10.11867/j.issn.1001-8166.2014.11.1294

References

[1] Chisholm S W. Oceanography: Stirring times in the southern ocean[J]. Nature, 2000, 407: 685-687.
[2] Jiao N, Herndl G J, Hansell D A, et al.Microbial production of recalcitrant dissolved organic matter: Long-term carbon storage in the global ocean[J]. Nature Reviews Microbiology, 2010, 8: 593-599.
[3] Wang P, Li Q, Tian J, et al.Long-term cycles in the carbon reservoir of the quaternary ocean: A perspective from the South China Sea[J]. National Science Review, 2014, 1: 119-143.
[4] Jiao N, Robinson C, Azam F, et al.Mechanisms of microbial carbon sequestration in the ocean—Future research directions[J]. Biogeosciences, 2014, 11(6): 5285-5306.
[5] Kuypers M M, Blokker P, Erbacher J, et al.Massive expansion of marine archaea during a mid-cretaceous oceanic anoxic event[J]. Science, 2001, 293: 92-95.
[6] Iverson V, Morris R M, Frazar C D, et al.Untangling genomes from metagenomes: Revealing an uncultured class of marine euryarchaeota[J]. Science, 2012, 335: 587-590.
[7] Xie W, Zhang C, Zhou X, et al.Salinity-dominated change in community structure and ecological function of archaea from the lower pearl river to coastal South China Sea[J]. Applied Microbiology and Biotechnology, 2014, 98(18): 7971-7982.
[8] Wang J, Zhang C, Hong Y. Tendency of TEX86 deficiency in the transitional zone between lower Pearl River estuary and coastal South China Sea: Impact of changing archaeal community structure[J].Chemical Geology, in revision.
[9] Luo G, Junium C K, Kump L R, et al.Shallow stratification prevailed for ~1700 to ~1300 Ma ocean: Evidence from organic carbon isotopes in the north China Craton[J]. Earth and Planetary Science Letters, 2014, 400: 219-232.
[10] Jia C, Huang J, Kershaw S, et al.Microbial response to limited nutrients in shallow water immediately after the end-Permian mass extinction[J]. Geobiology, 2012, 10(1): 60-71.
[11] Xie S, Pancost R D, Wang Y, et al.Cyanobacterial blooms tied to volcanism during the 5 My Permo-Triassic biotic crisis[J]. Geology, 2010, 38(5): 447-450.
Options
Outlines

/

〈 〉

Address: No. 8, Tianshui Middle Road, Lanzhou, Gansu
QQ：114723517
Tel：0931-8762293　E-mail：adearth@lzb.ac.cn
陇ICP备2021001824号-5　 甘公网安备62010202000687