Ciliates along oxyclines of permanently stratified marine water columns

Author Posting. © The Author(s), 2014. This is the author's version of the work. It is posted here by permission of John Wiley & Sons for personal use, not for redistribution. The definitive version was published in Journal of Eukaryotic Microbiology 61 (2014): 434-445, doi:10.1111/jeu.12122.Studies of microbial communities in areas of the world where permanent marine water column oxyclines exist suggest they are ‘hotspots’ of microbial activity, and that these water features and the anoxic waters below them are inhabited by diverse protist taxa, including ciliates. These communities have minimal taxonomic overlap with those in overlying oxic water columns. Some ciliate taxa have been detected in multiple locations where these stable water column oxyclines exist, however, differences in such factors as hydrochemistry in the habitats that have been studied suggest local selection for distinct communities. We compare published data on ciliate communities from studies of deep marine water column oxyclines in Caricao Basin, Venezuela, and the Black Sea, with data from coastal, shallower oxycline waters in Framvaren and Mariager fjords, and from several deep-sea hypersaline anoxic basins (DHABs) in the Eastern Mediterranean Sea. Putative symbioses between Bacteria, Archaea, and ciliates observed along these oxyclines suggests a strategy of cooperative metabolism for survival that includes chemosynthetic autotrophy and exchanges of metabolic intermediates or end products between hosts and their prokaryotic partners.Edgcomb’s Cariaco work was a collaboration with G. Taylor (Stony Brook U.) and S. Epstein (Northeastern U.) (MCB-0348407 to VE), her DHAB work was a collaboration with J.M. Bernhard (WHOI), K. Kormas (U. Thessaly), M. Yakimov (CNRS), and T. Stoeck (U. Kaiserslautern) (NSF OCE-0849578 to VE and JMB).2015-05-0

Supplementary Table 4A: Metatranscriptome data summary for cellular activities presented and statistics on sequencing and removal of potential contaminant sequences, FPKM values

Dataset: IODP360 - FPKM valuesSupplementary Table 4A: Metatranscriptome data summary for cellular activities presented and statistics on sequencing and removal of potential contaminant sequences: FPKM values. Samples taken on board of the R/V JOIDES Resolution between November 30, 2015 and January 30, 2016. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/812936NSF Division of Ocean Sciences (NSF OCE) OCE-165803

Supplementary Table 4B: Annotations for contigs within transcriptome libraries for the eleven samples that were manually curated for selected metabolic processes

Dataset: IODP360 - AnnotationsSupplementary Table 4B: Metatranscriptome data summary for cellular activities presented and statistics on sequencing and removal of potential contaminant sequences: Annotations for contigs within transcriptome libraries for the eleven samples that were manually curated for selected metabolic processes. Samples taken on board of the R/V JOIDES Resolution between November 30, 2015 and January 30, 2016. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/812997NSF Division of Ocean Sciences (NSF OCE) OCE-165803

Microbial hydrocarbon degradation in Guaymas Basin—exploring the roles and potential interactions of fungi and sulfate-reducing bacteria

© The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Edgcomb, V., Teske, A., & Mara, P. Microbial hydrocarbon degradation in Guaymas Basin—exploring the roles and potential interactions of fungi and sulfate-reducing bacteria. Frontiers in Microbiology, 13, (2022): 831828, https://doi.org/10.3389/fmicb.2022.831828.Hydrocarbons are degraded by specialized types of bacteria, archaea, and fungi. Their occurrence in marine hydrocarbon seeps and sediments prompted a study of their role and their potential interactions, using the hydrocarbon-rich hydrothermal sediments of Guaymas Basin in the Gulf of California as a model system. This sedimented vent site is characterized by localized hydrothermal circulation that introduces seawater sulfate into methane- and hydrocarbon-rich sediments, and thus selects for diverse hydrocarbon-degrading communities of which methane, alkane- and aromatics-oxidizing sulfate-reducing bacteria and archaea have been especially well-studied. Current molecular and cultivation surveys are detecting diverse fungi in Guaymas Basin hydrothermal sediments, and draw attention to possible fungal-bacterial interactions. In this Hypothesis and Theory article, we report on background, recent results and outcomes, and underlying hypotheses that guide current experiments on this topic in the Edgcomb and Teske labs in 2021, and that we will revisit during our ongoing investigations of bacterial, archaeal, and fungal communities in the deep sedimentary subsurface of Guaymas Basin.This project was supported by collaborative NSF Biological Oceanography grants OCE-1829903 and OCE-1829680 “Hydrothermal fungi in the Guaymas Basin Hydrocarbon Ecosystem” to VE and AT, and collaborative NSF Biological Oceanography grants OCE-2046799 and OCE-2048489 “IODP-enabled Insights into Fungi and Their Metabolic Interactions with Other Microorganisms in Deep Subsurface Hydrothermal Sediments” to VE and AT. PM was supported by OCE-2046799 and OCE-1829903. Sampling in Guaymas Basin was supported by collaborative NSF Biological Oceanography grant 1357238 “Collaborative Research: Microbial carbon cycling and its interaction with sulfur and nitrogen transformations in Guaymas Basin hydrothermal sediments” to AT

Editorial: Insights in extreme microbiology: 2022

Taking stock of the contributions to the “Insights in extreme microbiology: 2022” Research Topic again reveals the extraordinary breadth that exists within the field of Extreme Microbiology

Deep subsurface microbiology : a guide to the research topic papers

© The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 4 (2013): 122, doi:10.3389/fmicb.2013.00122.Deep subsurface microbiology is a rising field in geomicrobiology, environmental microbiology and microbial ecology that focuses on the molecular detection and quantification, cultivation, biogeographic examination, and distribution of bacteria, archaea, and eukarya that permeate the subsurface biosphere. The deep biosphere includes a variety of subsurface habitats, such as terrestrial deep aquifer systems or mines, deeply buried hydrocarbon reservoirs, marine sediments and the basaltic ocean crust. The deep subsurface biosphere abounds with uncultured, only recently discovered and—at best—incompletely understood microbial populations. So far, microbial cells and DNA remain detectable at sediment depths of more than 1 km and life appears limited mostly by heat in the deep subsurface. Severe energy limitation, either as electron acceptor or donor shortage, and scarcity of microbially degradable organic carbon sources are among the evolutionary pressures that may shape the genomic and physiological repertoire of the deep subsurface biosphere. Its biogeochemical importance in long-term carbon sequestration, subsurface elemental cycling and crustal aging, is a major focus of current research at the interface of microbiology, geochemistry, and biosphere/geosphere evolution

Gene expression in the deep biosphere

Author Posting. © The Author(s), 2013. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature 499 (2013): 205-208, doi:10.1038/nature12230.Scientific ocean drilling has revealed a deep biosphere of widespread microbial life in sub-seafloor sediment. Microbial metabolism in the marine subsurface likely plays an important role in global biogeochemical cycles1-3 but deep biosphere activities are not well understood1. Here, we describe and analyze the first subseafloor metatranscriptomes from anaerobic Peru Margin sediment up to 159 meters below seafloor (mbsf) represented by over 1 billion cDNA sequence reads. Anaerobic metabolism of amino acids, carbohydrates, and lipids appear to be dominant metabolic processes, and profiles of dissimilatory sulfite reductase (Dsr) transcripts are consistent with porewater sulfate concentration profiles1. Moreover, transcripts involved in cell division increase as a function of microbial cell concentration, indicating that increases in subseafloor microbial abundance are a function of cell division across all three domains of life. These data support calculations1 and models4 of subseafloor microbial metabolism and represent the first holistic picture of deep biosphere activities.This work was fostered by a Center for Dark Energy Biosphere Investigations (CDEBI) grant OCE-0939564 to WO and a NSF IOS grant 1238801 to JFB.2013-12-1

Microbial Hydrocarbon Degradation in Guaymas Basin—Exploring the Roles and Potential Interactions of Fungi and Sulfate-Reducing Bacteria

Hydrocarbons are degraded by specialized types of bacteria, archaea, and fungi. Their occurrence in marine hydrocarbon seeps and sediments prompted a study of their role and their potential interactions, using the hydrocarbon-rich hydrothermal sediments of Guaymas Basin in the Gulf of California as a model system. This sedimented vent site is characterized by localized hydrothermal circulation that introduces seawater sulfate into methane- and hydrocarbon-rich sediments, and thus selects for diverse hydrocarbon-degrading communities of which methane, alkane- and aromatics-oxidizing sulfate-reducing bacteria and archaea have been especially well-studied. Current molecular and cultivation surveys are detecting diverse fungi in Guaymas Basin hydrothermal sediments, and draw attention to possible fungal-bacterial interactions. In this Hypothesis and Theory article, we report on background, recent results and outcomes, and underlying hypotheses that guide current experiments on this topic in the Edgcomb and Teske labs in 2021, and that we will revisit during our ongoing investigations of bacterial, archaeal, and fungal communities in the deep sedimentary subsurface of Guaymas Basin

Phylogenetic position of parabasalid symbionts from the termite Calotermes flavicollis based on small subunit rRNA sequences

Small subunit rDNA genes were amplified by polymerase chain reaction using specific primers from mixed-population DNA obtained from the whole hindgut of the termite Calotermes flavicollis. Comparative sequence analysis of the clones revealed two kinds of sequences that were both from parabasalid symbionts. In a molecular tree inferred by distance, parsimony and likelihood methods, and including 27 parabasalid sequences retrieved from the data bases, the sequences of the group II (clones Cf5 and Cf6) were closely related to the Devescovinidae/Calonymphidae species and thus were assigned to the Devescovinidae Foaina. The sequence of the group I (clone Cf1) emerged within the Trichomonadinae and strongly clustered with Tetratrichomonas gallinarum. On the basis of morphological data, the Monocercomonadidae Hexamastix termitis might be the most likely origin of this sequence