Exploring Novel Interactions Between Microbes and Minerals

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Environmental Mineralogy and Biogeochemistry".

Deadline for manuscript submissions: 31 August 2025 | Viewed by 224

Special Issue Editor


E-Mail Website
Guest Editor
1. NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
2. Department of Astronomy, University of Maryland, College Park, Maryland, MD 20742, USA
Interests: lava tube biogeochemistry; biosignatures; biomineralization

Special Issue Information

Dear Colleagues,

Minerals are defined as inorganic, crystalline solids that form in many natural environments as a result of abiotic geochemical processes. Yet, for a wide variety of surface and near-surface environments on Earth, mineral formation occurs as a combination of both abiotic and biotic processes. Minerals provide energetically favorable substrates for microbes to establish communities in the form of biofilms or microbial mats; their metabolic processes, along with the cycling of decaying organic matter, result in cation and metal exchange between the microbes and minerals. This exchange induces changes to the chemical environment, which results in the formation of secondary minerals, such as clays, Fe-oxides/hydroxides, carbonates, or sulfates, on the original mineral substrates through bioweathering or on microbial materials through biomineralization. The minerals may incorporate microbial compounds within their structure or preserve morphologic features, such as microfossils. The microbial overprint on minerals in the rock record can become obscured depending on environmental conditions, making it challenging to discern biotic from abiotic minerals. To facilitate the distinction in their origins, a wide variety of laboratory and analytical techniques have been employed to study the surficial, structural, and chemical characteristics of the minerals as well as the metabolisms and organic compounds that are involved. Understanding the types of microbial signatures that are incorporated in minerals and how they evolve is essential for reconstructing past environments, understanding how compounds are cycled in the environment, and acknowledging what traces of life could be detectable on planetary bodies beyond Earth.

Dr. Dina M. Bower
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 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. Minerals is an international peer-reviewed open access monthly 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 2400 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

  • bioweathering
  • biomineralization
  • biogeochemistry
  • microbial mats
  • biofilms
  • secondary minerals
  • microfossils
  • metabolisms
  • biotic
  • abiotic

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Published Papers

This special issue is now open for submission.
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