Articles | Volume 19, issue 1
https://doi.org/10.5194/os-19-101-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-19-101-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
25 Jan 2023
Research article |
| 25 Jan 2023
| 25 Jan 2023
Unifying biological field observations to detect and compare ocean acidification impacts across marine species and ecosystems: what to monitor and why
Steve Widdicombe
Plymouth Marine Laboratory (PML), Plymouth, PL1 3DH, UK
Kirsten Isensee
Intergovernmental Oceanographic Commission of the United Nations
Educational, Scientific and Cultural Organization, Paris, 75732, France
Yuri Artioli
Plymouth Marine Laboratory (PML), Plymouth, PL1 3DH, UK
Juan Diego Gaitán-Espitia
The Swire Institute of Marine Science, School of Biological Sciences,
The Hong Kong University, Hong Kong, China
Claudine Hauri
International Arctic Research Center, University of Alaska Fairbanks,
Fairbanks, AK 99775-0100, USA
Janet A. Newton
Applied Physics Laboratory and College of the Environment, University
of Washington, Seattle, WA 98105-6698, USA
Mark Wells
School of Marine Sciences, The University of Maine, Orono, ME
04469-5706, USA
State Key Laboratory of Satellite Ocean Environment Dynamics, Second
Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China
Sam Dupont
CORRESPONDING AUTHOR
Department of Biological and Environmental Sciences, University of
Gothenburg, Fiskebäckskil, 45178, Sweden
Radioecology Laboratory International Atomic Energy Agency (IAEA),
Marine Laboratories, 98000, Principality of Monaco
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ERSEM 15.06 is a model for marine biogeochemistry and the lower trophic levels of the marine food web. It comprises a pelagic and benthic sub-model including the microbial food web and the major biogeochemical cycles of carbon, nitrogen, phosphorus, silicate, and iron using dynamic stochiometry. Further features include modules for the carbonate system and calcification. We present full mathematical descriptions of all elements along with examples at various scales up to 3-D applications.
Y. Artioli, J. C. Blackford, G. Nondal, R. G. J. Bellerby, S. L. Wakelin, J. T. Holt, M. Butenschön, and J. I. Allen
Biogeosciences, 11, 601–612, https://doi.org/10.5194/bg-11-601-2014, https://doi.org/10.5194/bg-11-601-2014, 2014
J. Holt, C. Schrum, H. Cannaby, U. Daewel, I. Allen, Y. Artioli, L. Bopp, M. Butenschon, B. A. Fach, J. Harle, D. Pushpadas, B. Salihoglu, and S. Wakelin
Biogeosciences Discuss., https://doi.org/10.5194/bgd-11-1909-2014, https://doi.org/10.5194/bgd-11-1909-2014, 2014
Revised manuscript not accepted
C. Hauri, N. Gruber, M. Vogt, S. C. Doney, R. A. Feely, Z. Lachkar, A. Leinweber, A. M. P. McDonnell, M. Munnich, and G.-K. Plattner
Biogeosciences, 10, 193–216, https://doi.org/10.5194/bg-10-193-2013, https://doi.org/10.5194/bg-10-193-2013, 2013
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Short summary
Ocean acidification is a global perturbation of the ocean carbonate chemistry as a consequence of increased carbon dioxide concentration in the atmosphere. While great progress has been made over the last decade for chemical monitoring, ocean acidification biological monitoring remains anecdotal. This is a consequence of a lack of standards, general methodological framework, and overall methodology. This paper presents methodology focusing on sensitive traits and rates of change.
Ocean acidification is a global perturbation of the ocean carbonate chemistry as a consequence...
