water-logo

Journal Browser

Journal Browser

Carbon Storage in Lake Sediments Under Climate Change

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Water and Climate Change".

Deadline for manuscript submissions: 30 December 2025 | Viewed by 321

Special Issue Editors


E-Mail Website
Guest Editor
Institute of Soil Science, Environment Engineering and Management, University of Life Sciences in Lublin, Leszczyńskiego 7, 20-069 Lublin, Poland
Interests: biochemical indicators of carbon transformations; cycle of carbon; enzymatic activity; dehydrogenases; urease; proteases; phosphatases; carbon sequestration; carbon stocks
Special Issues, Collections and Topics in MDPI journals

E-Mail Website
Guest Editor Assistant
Institute of Soil Science, Environmental Engineering and Management, University of Life Sciences in Lublin, Leszczyńskiego St. 7, 20-069 Lublin, Poland
Interests: sediments; floodplain lakes; dam reservoirs; Fluvisols; sediment chemistry; carbon stocks; humus substances

Special Issue Information

Dear Colleagues,

Limiting climate change is currently one of the most critical challenges facing science in the 21st century. Achieving this goal requires a comprehensive understanding of carbon resources and the mechanisms of carbon cycling in the environment. In this context, lake research plays a particularly important role. Lake sediments store substantial amounts of carbon, as demonstrated by numerous studies. However, lakes are especially vulnerable to climate change. Rising water temperatures, altered sedimentation patterns, and significant changes in water surface area and volume highlight the need to update and expand our understanding of these dynamic ecosystems. In this regard, it is of crucial importance to identify indicators of carbon transformation and storage rates in sediments, which will allow tracking the dynamics of carbon sequestration under increasing environmental changes.

We welcome submissions that explore how climate change influences carbon dynamics in lake sediments, including carbon stocks, carbon forms, carbon interactions between water and sediment, carbon exchanges between sediment and the atmosphere, biochemical indicators of carbon transformations in sediments, modelling of future changes, and the impact of these changes on society and industry.

We particularly encourage studies from diverse climatic zones to provide a broad perspective on these changes, deepen our understanding of the carbon cycle in lake sediments, and support efforts to mitigate climate change

Prof. Dr. Barbara Futa
Guest Editor

Dr. Joanna Gmitrowicz-Iwan
Guest Editor Assistant

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 100 words) can be sent to the Editorial Office for announcement on this website.

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. Water 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

  • carbon cycle
  • drought
  • lake
  • dam reservoir
  • carbon stocks
  • humus substances
  • fulvid and humic acids
  • sediments
  • indicators

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • Reprint: MDPI Books provides the opportunity to republish successful Special Issues in book format, both online and in print.

Further information on MDPI's Special Issue policies can be found here.

Published Papers (1 paper)

Order results
Result details
Select all
Export citation of selected articles as:

Research

13 pages, 1249 KB  
Article
Geochemical and Mineralogical Characterisation of Carbonate-Rich Lake Sediments from Lake Kolon, Hungary
by Tamás Zsolt Vári, Gábor Bozsó, Pál Sümegi and Elemér Pál-Molnár
Water 2025, 17(19), 2830; https://doi.org/10.3390/w17192830 - 26 Sep 2025
Abstract
The Danube–Tisza Interfluve in central Hungary, a key region for Quaternary paleoenvironmental reconstruction, hosts ephemeral saline lakes that serve as highly sensitive archives of past climate variability but are increasingly threatened by desertification. Carbonate-rich lacustrine deposits within these systems form through a complex [...] Read more.
The Danube–Tisza Interfluve in central Hungary, a key region for Quaternary paleoenvironmental reconstruction, hosts ephemeral saline lakes that serve as highly sensitive archives of past climate variability but are increasingly threatened by desertification. Carbonate-rich lacustrine deposits within these systems form through a complex interplay of biogenic CO2 uptake and inorganic precipitation driven by evaporation. To refine paleoenvironmental reconstructions from these archives, a lacustrine sediment core was analysed using XRPD for mineralogy and XRF for major and trace element geochemistry. The results reveal four distinct environmental phases: a cold, siliciclastic-dominated Late Glacial period (c. 23,600–13,400 cal BP); an abrupt shift to massive autogenic carbonate production during the warmer Late Glacial Interstadial, which was also marked by intense aeolian activity (Zr enrichment); the development of a Holocene fen (from c. 11,200 cal BP) with fluctuating hydrology; and a recent interval (from c. 800 cal BP) showing extreme enrichment in phosphorus, lead, and sulphur from anthropogenic sources. Full article
(This article belongs to the Special Issue Carbon Storage in Lake Sediments Under Climate Change)
Show Figures

Figure 1

Back to TopTop