The 10th Anniversary of the "Chemical Oceanography" Section

A special issue of Journal of Marine Science and Engineering (ISSN 2077-1312). This special issue belongs to the section "Chemical Oceanography".

Deadline for manuscript submissions: closed (31 December 2025) | Viewed by 1423

Special Issue Editor

Special Issue Information

Dear Colleagues,

Journal of Marine Science and Engineering is going to reach a remarkable milestone, and in celebration of this special occasion, we have taken the initiative to launch a Special Issue called “The 10th Anniversary of the 'Chemical Oceanography' Section”.

The Special Issue aims to gather moderate-sized original research or review papers featuring important and recent developments or recent progress in chemical oceanography and welcomes studies on the following:

  • The interactions between seawater, the atmosphere, the seafloor, and marine organisms.
  • Cycling of elements like carbon, nitrogen, and phosphorus as well as their interactions, transformational processes, carbon sequestration, ocean acidification, and effects on aquatic biota.
  • The behaviour of trace metals, and the study of gases and nutrients in marine environments and ocean circulation.
  • The interaction of organic and inorganic molecules, particulate and dissolved matter, and ocean sediments.
  • The effects of human activities, such as pollution and climate change, on oceanic systems.

In order to comprehend the factors influencing chemical compositions and how they change over time and space, the papers may discuss experimental or field research in settings like salt marshes, deep ocean sediments, cold seeps, and saline lakes. They may also combine field observations, laboratory experiments, and computer models.

Ultimately, attention will be focused on analytical chemistry of the oceans, anthropogenic climate change, and restoring the chemistry of the oceans.

Potential authors should be well-known experts in their domain and are invited to submit their contributions at any time from now until the submission deadline.

Prof. Dr. Michele Arienzo
Guest Editor

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 250 words) can be sent to the Editorial Office for assessment.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Journal of Marine Science and Engineering is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2600 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • sources and flows of elements in oceans
  • characterization and quantification of elements in marine waters
  • interaction of elements with suspended particulate, seafloor, and marine biota and xenobiotics
  • fate and effects of elements and organics with marine biota and modelling
  • current challenges and future solutions for prevention, mitigation strategies and remediation of ocean ecological systems
  • carbon sequestration and ocean acidification
  • the effects of human activities, such as pollution and climate change, on oceanic systems
  • anthropogenic climate change and restoring the chemistry of the oceans

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Published Papers (1 paper)

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Research

25 pages, 8612 KB  
Article
Effect of Wind-Driven Circulation on the Spatial Distribution of Dissolved Oxygen and Carbonate System Variables in the Mexican Tropical Pacific Region
by Asbel Itahi de la Cruz-Ruiz, Luis A. Soto-Mardones, Cecilia Chapa-Balcorta, Teresa Leticia Espinosa-Carreón, Claudia E. Aburto-Leiva, José Martín Hernández-Ayón, Luz de Lourdes Aurora Coronado-Álvarez, Víctor Hugo Martínez-Magaña, María Luisa Leal-Acosta and Aurélien Paulmier
J. Mar. Sci. Eng. 2026, 14(5), 514; https://doi.org/10.3390/jmse14050514 - 9 Mar 2026
Viewed by 940
Abstract
The Mexican Tropical Pacific (MTP) is a key component of the Eastern Tropical North Pacific Oxygen Minimum Zone, yet its carbonate system variability remains poorly constrained. This study examines wind-driven circulation effects on dissolved oxygen (DO) and the carbonate system —dissolved inorganic carbon [...] Read more.
The Mexican Tropical Pacific (MTP) is a key component of the Eastern Tropical North Pacific Oxygen Minimum Zone, yet its carbonate system variability remains poorly constrained. This study examines wind-driven circulation effects on dissolved oxygen (DO) and the carbonate system —dissolved inorganic carbon (DIC), total alkalinity (TA), total-scale pH (pHT), partial pressure of CO2 in seawater (pCO2w) and air–sea CO2 fluxes (FCO2)— in the Gulf of Tehuantepec (GT) and Tehuantepec Bowl (TB). Hydrographic data and discrete water samples were collected at 50 oceanographic stations during March 2020. Principal Component Analysis (PCA) identifies wind-driven circulation as the primary control of biogeochemical variability. Tehuano wind events and mesoscale eddies promoted upwelling of low-oxygen (DO < 20 µmol kg−1) and high-DIC (>2200 µmol kg−1) waters to 50 m depth in the central GT, while downwelling conditions prevailed in the TB. Stoichiometric analysis revealed DIC-DO coupling (slope = −1.39). Overall, the MTP acted as CO2 source (FCO2 ranging from −1.92 to 24.11 mmol m−2 d−1), with enhanced emissions linked to eddy-induced upwelling. This study provides the first integrated characterization of the carbonate system across both the GT and TB. Full article
(This article belongs to the Special Issue The 10th Anniversary of the "Chemical Oceanography" Section)
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