scholarly journals Archaeal and Bacterial Glycerol Dialkyl Glycerol Tetraether Lipids in Hot Springs of Yellowstone National Park

2007 ◽  
Vol 73 (19) ◽  
pp. 6181-6191 ◽  
Author(s):  
Stefan Schouten ◽  
Marcel T. J. van der Meer ◽  
Ellen C. Hopmans ◽  
W. Irene C. Rijpstra ◽  
Anna-Louise Reysenbach ◽  
...  
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Hot Springs ◽  
Membrane Lipids ◽  
Hot Spring ◽  
Ph Values ◽  
Group I ◽  
Low Concentrations ◽  
Tetraether Lipids

ABSTRACTGlycerol dialkyl glycerol tetraethers (GDGTs) are core membrane lipids originally thought to be produced mainly by (hyper)thermophilic archaea. Environmental screening of low-temperature environments showed, however, the abundant presence of structurally diverse GDGTs from both bacterial and archaeal sources. In this study, we examined the occurrences and distribution of GDGTs in hot spring environments in Yellowstone National Park with high temperatures (47 to 83°C) and mostly neutral to alkaline pHs. GDGTs with 0 to 4 cyclopentane moieties were dominant in all samples and are likely derived from both (hyper)thermophilicCrenarchaeotaandEuryarchaeota. GDGTs with 4 to 8 cyclopentane moieties, likely derived from the crenarchaeotal orderSulfolobalesand the euryarchaeotal orderThermoplasmatales, are usually present in much lower abundance, consistent with the relatively high pH values of the hot springs. The relative abundances of cyclopentane-containing GDGTs did not correlate with in situ temperature and pH, suggesting that other environmental and possibly genetic factors play a role as well. Crenarchaeol, a biomarker thought to be specific for nonthermophilic group ICrenarchaeota, was also found in most hot springs, though in relatively low concentrations, i.e., <5% of total GDGTs. Its abundance did not correlate with temperature, as has been reported previously. Instead, the cooccurrence of relatively abundant nonisoprenoid GDGTs thought to be derived from soil bacteria suggests a predominantly allochthonous source for crenarchaeol in these hot spring environments. Finally, the distribution of bacterial branched GDGTs suggests that they may be derived from the geothermally heated soils surrounding the hot springs.

scholarly journals Fungi from Geothermal Soils in Yellowstone National Park

1999 ◽  
Vol 65 (12) ◽  
pp. 5193-5197 ◽  
Author(s):  
Regina S. Redman ◽  
Anastassia Litvintseva ◽  
Kathy B. Sheehan ◽  
Joan M. Henson ◽  
Rusty J. Rodriguez
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Hot Springs ◽  
Root Zone ◽  
Fungal Species ◽  
Sparse Vegetation ◽  
Perennial Plant ◽  
Ph Values ◽  
Geothermal Soils

ABSTRACT Geothermal soils near Amphitheater Springs in Yellowstone National Park were characterized by high temperatures (up to 70°C), high heavy metal content, low pH values (down to pH 2.7), sparse vegetation, and limited organic carbon. From these soils we cultured 16 fungal species. Two of these species were thermophilic, and six were thermotolerant. We cultured only three of these species from nearby cool (0 to 22°C) soils. Transect studies revealed that higher numbers of CFUs occurred in and below the root zone of the perennial plant Dichanthelium lanuginosum (hot springs panic grass). The dynamics of fungal CFUs in geothermal soil and nearby nongeothermal soil were investigated for 12 months by examining soil cores and in situ mesocosms. For all of the fungal species studied, the temperature of the soil from which the organisms were cultured corresponded with their optimum axenic growth temperature.

scholarly journals Pyrobaculum yellowstonensis Strain WP30 Respires on Elemental Sulfur and/or Arsenate in Circumneutral Sulfidic Geothermal Sediments of Yellowstone National Park

2015 ◽  
Vol 81 (17) ◽  
pp. 5907-5916 ◽  
Author(s):  
Z. J. Jay ◽  
J. P. Beam ◽  
A. Dohnalkova ◽  
R. Lohmayer ◽  
B. Bodle ◽  
...  
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Elemental Sulfur ◽  
De Novo ◽  
Hot Spring ◽  
Content Type ◽  
Physiological Attributes ◽  
And Function ◽  
Metagenome Sequence

ABSTRACTThermoproteales(phylumCrenarchaeota) populations are abundant in high-temperature (>70°C) environments of Yellowstone National Park (YNP) and are important in mediating the biogeochemical cycles of sulfur, arsenic, and carbon. The objectives of this study were to determine the specific physiological attributes of the isolatePyrobaculum yellowstonensisstrain WP30, which was obtained from an elemental sulfur sediment (Joseph's Coat Hot Spring [JCHS], 80°C, pH 6.1, 135 μM As) and relate this organism to geochemical processes occurringin situ. Strain WP30 is a chemoorganoheterotroph and requires elemental sulfur and/or arsenate as an electron acceptor. Growth in the presence of elemental sulfur and arsenate resulted in the formation of thioarsenates and polysulfides. The complete genome of this organism was sequenced (1.99 Mb, 58% G+C content), revealing numerous metabolic pathways for the degradation of carbohydrates, amino acids, and lipids. Multiple dimethyl sulfoxide-molybdopterin (DMSO-MPT) oxidoreductase genes, which are implicated in the reduction of sulfur and arsenic, were identified. Pathways for thede novosynthesis of nearly all required cofactors and metabolites were identified. The comparative genomics ofP. yellowstonensisand the assembled metagenome sequence from JCHS showed that this organism is highly related (∼95% average nucleotide sequence identity) toin situpopulations. The physiological attributes and metabolic capabilities ofP. yellowstonensisprovide an important foundation for developing an understanding of the distribution and function of these populations in YNP.

scholarly journals Nanoarchaeota, Their Sulfolobales Host, and Nanoarchaeota Virus Distribution across Yellowstone National Park Hot Springs

2015 ◽  
Vol 81 (22) ◽  
pp. 7860-7868 ◽  
Author(s):  
Jacob H. Munson-McGee ◽  
Erin K. Field ◽  
Mary Bateson ◽  
Colleen Rooney ◽  
Ramunas Stepanauskas ◽  
...  
Keyword(s):  
Single Cell ◽  
Yellowstone National Park ◽  
National Park ◽  
Hot Springs ◽  
Hot Spring ◽  
Genome Comparison ◽  
Fish Analysis ◽  
Content Type ◽  
Cell Genome ◽  
Single Cell Genome

ABSTRACTNanoarchaeotaare obligate symbionts with reduced genomes first described from marine thermal vent environments. Here, both community metagenomics and single-cell analysis revealed the presence ofNanoarchaeotain high-temperature (∼90°C), acidic (pH ≈ 2.5 to 3.0) hot springs in Yellowstone National Park (YNP) (United States). Single-cell genome analysis of two cells resulted in two nearly identical genomes, with an estimated full length of 650 kbp. Genome comparison showed that these two cells are more closely related to the recently proposedNanobsidianus stetterifrom a more neutral YNP hot spring than to the marineNanoarchaeum equitans. Single-cell and catalyzed reporter deposition-fluorescencein situhybridization (CARD-FISH) analysis of environmental hot spring samples identified the host of the YNPNanoarchaeotaas aSulfolobalesspecies known to inhabit the hot springs. Furthermore, we demonstrate thatNanoarchaeotaare widespread in acidic to near neutral hot springs in YNP. An integrated viral sequence was also found within oneNanoarchaeotasingle-cell genome and further analysis of the purified viral fraction from environmental samples indicates that this is likely a virus replicating within the YNPNanoarchaeota.

scholarly journals Characterizing and Evaluating the Diverse Microbial Communities and Their Mercury Resistance Potential from Hot Spring Sites Representing Gradients in Temperature and pH in Yellowstone National Park

2020 ◽  
Vol 1 (1) ◽  
Author(s):  
Yelizaveta Rassadkina ◽  
Spencer Roth ◽  
Tamar Barkay
Keyword(s):  
Microbial Communities ◽  
Yellowstone National Park ◽  
National Park ◽  
Hot Springs ◽  
Hot Spring ◽  
Thermophilic Bacteria ◽  
Sequence Data ◽  
Mercury Resistance ◽  
Sample Site ◽  
Microorganism Community

Yellowstone National Park is home to many different hot springs, lakes, geysers, pools, and basins that range in pH, chemical composition, and temperature. These different environmental variations provide a broad range of conditions that select and grow diverse communities of microorganisms. In this study, we collected samples from geochemically diverse lakes and springs to characterize the microbial communities present through 16S rRNA metagenomic analysis. This information was then used to observe how various microorganisms survive in high mercury environments. The results show the presence of microorganisms that have been studied in previous literature. The results also depict gradients of microorganisms including thermophilic bacteria and archaea that exist in these extreme environments. In addition, beta diversity analyses of the sequence data showed site clustering based primarily on temperature instead of pH or sample site, suggesting that while pH, temperature, and sample site were all shown to be significant, temperature is the strongest factor driving microorganism community development. While it is important to characterize the microorganism community present, it is also important to understand how this community functions as a result of its selection. Along with looking at community composition, genomic material was tested to see if it contained mercury methylating (hgcA) or mercury reducing (merA) genes. Out of 22 samples, three of them were observed to have merA genes, while no samples had hgcA genes. These results indicate that microorganisms in Mustard and Nymph Springs may use mercury reduction. Understanding how microorganisms survive in environments with high concentrations of toxic pollutants is crucial because it can be used as a model to better understand mechanisms of resistance and the biogeochemical cycle, as well as for bioremediation and other solutions to anthropogenic problems.

scholarly journals Stable Isotope Probing for Microbial Iron Reduction in Chocolate Pots Hot Spring, Yellowstone National Park

2018 ◽  
Vol 84 (11) ◽  
Author(s):  
Nathaniel W. Fortney ◽  
Shaomei He ◽  
Ajinkya Kulkarni ◽  
Michael W. Friedrich ◽  
Charlotte Holz ◽  
...  
Keyword(s):  
Microbial Community ◽  
Stable Isotope ◽  
Yellowstone National Park ◽  
National Park ◽  
Hot Spring ◽  
Redox Cycling ◽  
Stable Isotope Probing ◽  
Content Type ◽  
Insight Into

ABSTRACTChocolate Pots hot springs (CP) is a circumneutral-pH Fe-rich geothermal feature located in Yellowstone National Park. Previous Fe(III)-reducing enrichment culture studies with CP sediments identified close relatives of known dissimilatory Fe(III)-reducing bacterial (FeRB) taxa, includingGeobacterandMelioribacter. However, the abundances and activities of such organisms in the native microbial community are unknown. Here, we used stable isotope probing experiments combined with 16S rRNA gene amplicon and shotgun metagenomic sequencing to gain an understanding of thein situFe(III)-reducing microbial community at CP. Fe-Si oxide precipitates collected near the hot spring vent were incubated with unlabeled and13C-labeled acetate to target active FeRB. We searched reconstructed genomes for homologs of genes involved in known extracellular electron transfer (EET) systems to identify the taxa involved in Fe redox transformations. Known FeRB taxa containing putative EET systems (Geobacter,Ignavibacteria) increased in abundance under acetate-amended conditions, whereas genomes related toIgnavibacteriumandThermodesulfovibriothat contained putative EET systems were recovered from incubations without electron donor. Our results suggest that FeRB play an active role in Fe redox cycling within Fe-Si oxide-rich deposits located at the hot spring vent.IMPORTANCEThe identification of past near-surface hydrothermal environments on Mars emphasizes the importance of using modern Earth environments, such as CP, to gain insight into potential Fe-based microbial life on other rocky worlds, as well as ancient Fe-rich Earth ecosystems. By combining stable carbon isotope probing techniques and DNA sequencing technology, we gained insight into the pathways of microbial Fe redox cycling at CP. The results suggest that microbial Fe(III) oxide reduction is prominentin situ, with important implications for the generation of geochemical and stable Fe isotopic signatures of microbial Fe redox metabolism within Fe-rich circumneutral-pH thermal spring environments on Earth and Mars.

Evidence for high-temperature in situ nifH transcription in an alkaline hot spring of Lower Geyser Basin, Yellowstone National Park

2012 ◽  
Vol 14 (5) ◽  
pp. 1272-1283 ◽  
Author(s):  
Sara T. Loiacono ◽  
D'Arcy R. Meyer-Dombard ◽  
Jeff R. Havig ◽  
Amisha T. Poret-Peterson ◽  
Hilairy E. Hartnett ◽  
...  
Keyword(s):  
High Temperature ◽  
Yellowstone National Park ◽  
National Park ◽  
Hot Spring

scholarly journals Molecular Characterization of Novel Red Green Nonsulfur Bacteria from Five Distinct Hot Spring Communities in Yellowstone National Park

2002 ◽  
Vol 68 (1) ◽  
pp. 346-355 ◽  
Author(s):  
Sarah M. Boomer ◽  
Daniel P. Lodge ◽  
Bryan E. Dutton ◽  
Beverly Pierson
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Hot Springs ◽  
Hot Spring ◽  
Site Specificity ◽  
Absorption Bands ◽  
Specific Primers ◽  
In Vivo Absorption

ABSTRACT We characterized and compared five geographically isolated hot springs with distinct red-layer communities in Yellowstone National Park. Individual red-layer communities were observed to thrive in temperatures ranging from 35 to 60°C and at pH 7 to 9. All communities were dominated by red filamentous bacteria and contained bacteriochlorophyll a (Bchl a), suggesting that they represented novel green nonsulfur (GNS) bacteria. The in vivo absorption spectra of individual sites were different, with two sites showing unusual Bchl a protein absorption bands beyond 900 nm. We prepared and analyzed 16S rRNA libraries from all of these sites by using a combination of general bacterial primers and new GNS-specific primers described here. These studies confirmed the presence of novel GNS-like bacteria in all five communities. All GNS-like clones were most similar to Roseiflexus castenholzii, a red filamentous bacterium from Japan that also contains only Bchl a. Phylogenies constructed by using GNS-like clones from Yellowstone red-layer communities suggest the presence of a moderately diverse new “red” cluster within the GNS lineage. Within this cluster, at least two well-supported subclusters emerged: YRL-A was most similar to Roseiflexus and YRL-B appeared to be novel, containing no known isolates. While these patterns showed some site specificity, they did not correlate with observed Bchl a spectrum differences or obvious features of the habitat.

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