- freely available
Biology 2013, 2(2), 798-809; doi:10.3390/biology2020798
Published: 30 May 2013
Abstract: Fumarolic Ice caves on Antarctica’s Mt. Erebus contain a dark oligotrophic volcanic ecosystem (DOVE) and represent a deep biosphere habitat that can provide insight into microbial communities that utilize energy sources other than photosynthesis. The community assembly and role of fungi in these environments remains largely unknown. However, these habitats could be relatively easily contaminated during human visits. Sixty-one species of fungi were identified from soil clone libraries originating from Warren Cave, a DOVE on Mt. Erebus. The species diversity was greater than has been found in the nearby McMurdo Dry Valleys oligotrophic soil. A relatively large proportion of the clones represented Malassezia species (37% of Basidomycota identified). These fungi are associated with skin surfaces of animals and require high lipid content for growth, indicating that contamination may have occurred through the few and episodic human visits in this particular cave. These findings highlight the importance of fungi to DOVE environments as well as their potential use for identifying contamination by humans. The latter offers compelling evidence suggesting more strict management of these valuable research areas.
The subsurface biosphere has been among the most exciting, and rapidly evolving research ecosystem types in biogeosciences of the past 20 years . Trace fossils of microbial dissolution in seafloor volcanic rocks suggest the presence of a Dark Oligotrophic Volcanic Ecosystem (DOVE) at least for the upper 500 m and extending back to first appearance of life on Planet Earth . DOVEs take a special role in the study of the subsurface biosphere. They are volumetrically very significant and they contain abundant energy donors from the earth’s interior, in the form of minerals and glasses that are highly reactive in low temperature hydrous environments. DOVEs commonly have active hydrothermal systems that readily circulate surface water and atmospheric gases through the interior of these volcanoes. The combination of surface-derived fluids and volcanic rocks from the interior of the earth providing abundant and effective combinations of electron acceptors and donors that can facilitate chemolithoautotrophic conditions for microbial communities to thrive without photosynthesis. Conditions of (near-) atmospheric oxygenation exist in very large fractions of DOVEs where water or air circulates relatively freely and recharges hydrothermal systems in active systems. These factors combine to make DOVEs a significant component of the subsurface biosphere and open up the possibility that DOVEs might provide biomass to the earth’s surface offering a “rock bottom” for the food web.
The southernmost active volcano in the world, Mt. Erebus (3,795 m), has been the focus of research for decades . Recently, ice caves and fumarolic ice towers near the summit have been recognized as a unique environment devoid of light and/or having a moist warm environment . These sub-glacial fumaroles issue gases that are dominated by air with 80–100% humidity and up to 2% CO2 [3,4]. CO2 is one of the few sources of carbon available to these microbial communities, although small amounts of organic carbon may enter the cave through melt water from the surface during the summer months that can contain algae or wind delivered carbon sources.
Some of the Mt. Erebus DOVEs are now visited more frequently yet others still remain pristine environments and there is a need to determine which caves are best suited for future microbiological research through a microbial community survey to determine if there has been anthropogenic intrusion on these communities. Since the earliest days of Mt. Erebus cave research, ice caves were thought of as naturally protected environments to be used for the placement of experiments, storing gear and even food. There is even the possibly that members of Antarctic Heroic Age explorers from either the Nimrod Expedition (1907–1909) with the first ascent in 1908 or the Terra Nova Expedition (1910–1913) with the highest camp up to that time, left food or materials near the caves. Establishment of McMurdo Station in 1956 by the US Navy helped increase the access to Mt. Erebus and continuous research began in the early 1970’s. One prominent Mt. Erebus cave, Warren Cave, is located in a logistically particularly strategic location, on a straight line between a recently discovered location of a camp by the Terra Nova Expedition (December 1912) and the summit of Mt. Erebus. This site is very close to Lower Erebus Hut, the operational base for the bulk of current research on Mt. Erebus.
The role of fungi in the DOVE communities is a new field of research and this is the first report of a fungal community associated with an Antarctic fumarole DOVE habitat.
2. Experimental Section
Sample site: Warren Cave on Mt. Erebus, Antarctica (77° 31.003 S; 167° 09.884 E) (Figure 1) has been visited by researchers annually over the past decade for the study of volcanic CO2 emissions and temperature fluctuations by the Mount Erebus Volcano Observatory (MEVO) . Warren Cave maintains a remarkably constant temperature. Temperatures in the fumarole studied were 18.5 °C inside the soil and 14.5 °C above the soil.
Sample collection: Soil substrate collected in 2010 from Warren Cave was taken from within a fumarolic vent issuing warm gas from beneath a protruding rock consisting of a patch of soil made up largely from coarse sand and fine gravel sized rock fragments (location labeled “GV 1” in ). The sample (Identification number: 10G439-WC) consisted of several pooled 10–15 g scoops collected aseptically in a sterile 50 mL tube. The sample was transported to the US at −20 °C. Soil temperature at the time of collection was 18.5 °C, the air temperature was 14.6 °C and soil pH was 5.2.
Soil analysis: Both soil moisture and carbon analyses were conducted by the University of Maine Analytical and Soil Testing Laboratory (Orono, ME, USA). Soil moisture was determined by gravimetric method at the time of soil drying for carbon analysis. Both total carbon and organic carbon were determined using the dry combustion method  with an Leco CN-2000 Carbon/Nitrogen analyzer.
Nucleic acid extraction and analysis: DNA from 1.62 g of the soil pellet was extracted using a ZR Soil Microbe Midi kit (Zymo Research, Irvine, CA, USA). The soil pellet was extracted 2× and the DNA was pooled. Three pellets were extracted for each clone library. Specific ITS region amplicons were produced by PCR (100 ng/reaction) in 25 μL reactions using Illustra PuReTaq Ready-To-Go™ PCR Beads (GE Lifesciences, Piscataway, NJ, USA). PCR primer set ITS5/ITS4  was used to target the ITS region for clone library construction. Initial denaturation was for 2 min at 95 °C and 35 cycles with a PTC-200 thermal cycler (MJ Research, Watertown, MA, USA) under the following conditions: 30 s at 95 °C, 30 s at 52.3 °C, 1 min at 72 °C with a final 72 °C 10 min extension. The resulting PCR products were cleaned prior to cloning using Promega SV Gel and PCR Clean-up System (Promega, Madison, WI, USA). Three PCR reactions were produced from each soil pellet DNA aliquot and pooled prior to library construction. Two ITS clone libraries ligations were produced. PCR products from multiple (4–8) clean PCR reactions (i.e., showing only bands within expected ITS size ranges) were pooled, and purified using a PCR purification kit (QIAGEN, Valencia, CA, USA). Libraries were generated using a TOPO TA cloning kit and chemically competent Escherichia coli TOP10F cells (Invitrogen, Carlsbad, CA, USA). The High Throughput Genomic Unit (HTGU—University of Washington, Seattle, WA, USA) preformed the transformations, clone selection and sequencing using the vector T7 primer. The resulting data were screened for (1) poor quality sequence (below 80% quality) and (2) short sequences (shorter than 400 bp) using Sequencher v 5.0.1 (Gene Codes Corp.) and these sequences were eliminated from further analysis. Sequences that passed the first two steps were then screened for chimeric sequences using Chimera Checker  and chimeric sequences were eliminated from further analysis. Each remaining sequence was reviewed by hand and compared with NCIB database (BLAST and Tree Builder) for taxonomic assignments. Based on suggestion of Fell and coworkers  sequence homology of >98% were considered to be the same species. GenBank accession numbers are shown in Table 1 and can be accessed through GenBank. The closest match isolates selected for Table 1 are comprised only of fungi that have been cultured.
|Table 1. Clones identified from Warren Cave with GenBank accession numbers and closest matches. Asterisks identify clones that fall below the 98% species identification threshold.|
|Warren Cave Clone Species||GenBank Accession Number||GenBank Closest Match||% match||GenBank Closest Match Species|
|Acremonium implicatum||KC785536||JQ692168||99%||Acremonium implicatum|
|* Acremonium sp.||KC785537||AB540571||94%||Acremonium cereale|
|Alternaria alternata||KC785538||AF218791||99%||Alternaria alternata|
|Aspergillus penicillioides||KC785539||HQ914939||99%||Aspergillus penicillioides|
|Aureobasidium pullulans||KC785542||FN868454||99%||Aureobasidium pullulans|
|Aureobasidium sp.||KC785543||HQ631013||99%||Aureobasidium sp. TMS-2011|
|Candida zeylanoides||KC785544||EF687774||100%||Candida zeylanoides|
|Cladosporium sp. 1||KC785545||HQ631003||100%||Cladosporium sp. TMS-2011 voucher|
|Cladosporium grevilleae||KC785546||JF770450||99%||Cladosporium grevilleae|
|Clavispora lusitaniae||KC785548||EU149777||99%||Clavispora lusitaniae|
|Cochliobolus lunatus||KC785549||HQ607915||100%||Cochliobolus lunatus|
|Cyphellophora laciniata||KC785550||EU035416||99%||Cyphellophora laciniata|
|Epicoccum nigrum||KC785551||HQ607859||100%||Epicoccum nigrum|
|Erysiphe polygoni||KC785552||AF011308||99%||Erysiphe polygoni|
|Gibellulopsis nigrescens||KC785553||KC156644||99%||Gibellulopsis nigrescens|
|*Hansfordia sp.||KC785554||HQ914948||96%||Hansfordia sp.|
|Lewia infectoria||KC785556||AY154718||99%||Lewia infectoria|
|Myrothecium verrucaria||KC785557||FJ235085||99%||Myrothecium verrucaria|
|Penicillium oxalicum||KC785558||JX231003||99%||Penicillium oxalicum|
|*Pezizomycotina sp.||KC785559||EU167561||96%||Pleiochaeta ghindensis|
|Phaeococcomyces nigricans||KC785560||AY843154||99%||Phaeococcomyces nigricans|
|Phaeosphaeria sp.||KC785561||HQ631018||99%||Phaeosphaeria sp. 1 TMS-2011 voucher|
|*Phialosimplex sp.||KC785562||GQ169326||93%||Phialosimplex chlamydosporus|
|Pleosporales sp.||KC785563||HQ207041||100%||Pleosporales sp. 24 PH|
|Saccharomyces cerevisiae||KC785564||AY939814||99%||Saccharomyces cerevisiae|
|Tetracladium sp. 1||KC785565||JF911760||98%||Tetracladium sp. QH32|
|Tetracladium sp. 2||KC785555||AB776690||99%||Tetracladium sp. SMU-1|
|Toxicocladosporium irritans||KC785566||EU040243||99%||Toxicocladosporium irritans|
|Verticillium dahliae||KC785567||HQ839784||99%||Verticillium dahliae|
|Volutella colletotrichoides||KC785568||AJ301962||100%||Volutella colletotrichoides|
|Ceriporiopsis subvermispora||KC785569||FJ713106||99%||Ceriporiopsis subvermispora|
|Cryptococcus wieringae||KC785570||FN824493||99%||Cryptococcus wieringae|
|Cystofilobasidium macerans||KC785572||AF444317||100%||Cystofilobasidium macerans|
|Endophyte sp.||KC785573||EU977202||99%||Fungal Endophyte sp. P807B|
|Exidia glandulosa||KC785574||AY509555||99%||Exidia glandulosa|
|*Exobasidium sp.||KC785575||EU784219||92%||Exobasidium rhododendri|
|Filobasidium floriforme||KC785576||AF190007||99%||Filobasidium floriforme|
|Ganoderma applanatum||KC785577||JX501311||99%||Ganoderma applanatum|
|Glaciozyma watsonii||KC785578||AY040660||99%||Glaciozyma watsonii|
|*Hymenochaete sp.||KC785579||JN230420||97%||Hymenochaete corrugata|
|Hyphodontia rimosissima||KC785580||DQ873627||99%||Hyphodontia rimosissima|
|Irpex lacteus||KC785581||EU273517||99%||Irpex lacteus|
|Malassezia globosa||KC785582||KC152884||99%||Malassezia globosa|
|Malassezia restricta||KC785583||EU400587||99%||Malassezia restricta|
|*Malassezia sp.||KC785585||KC141977||82%||Malassezia sympodialis|
|Mycena sp.||KC785587||JQ272379||99%||Mycena sp. 1 RB-2011|
|Peniophora lycii||KC785588||JX046435||99%||Peniophora lycii|
|*Phanerochaete sp.||KC785589||GU934592||96%||Phanerochaete sp. 853|
|*Polyporus sp.||KC785590||AF516599||97%||Polyporus tuberaster|
|Resinicium bicolor||KC785591||DQ826534||99%||Resinicium bicolor|
|Rhodotorula mucilaginosa||KC785592||HQ702343||99%||Rhodotorula mucilaginosa|
|Sistotrema brinkmanii||KC785594||DQ899095||99%||Sistotrema brinkmannii|
|Skeletocutis chrysella||KC785595||FN907916||99%||Skeletocutis chrysella|
|Sporobolomyces sp.||KC785596||EU002899||99%||Sporobolomyces sp.|
|Stereum sanguinolentum||KC785597||AY089730||99%||Stereum sanguinolentum|
|*Stereum sp.||KC785598||FN539049||91%||Stereum rugosum|
|Trametes cubensis||KC785599||JN164923||99%||Trametes cubensis|
|*Trichaptum sp.||KC785600||U63473||95%||Trichaptum biforme|
|*Ustilago sp.||KC785601||AY740170||97%||Ustilago drakensbergiana|
|Ustilago tritici||KC785602||JN114419||99%||Ustilago tritici|
Community analysis: The resulting passed sequences were classified into groups based on their phyla. Each group of sequences was aligned using MUSCLE web server alignment . The alignments were used to create phylogenetic trees through the Seaview software program, version 4.3.1. A rooted neighbor-joining distance tree was generated, for each phyla separately (Ascomycetes and Basidiomycetes), based on nucleotide positions of the ITS region of the 5.8S gene. Bootstrap values were based on 100 replicates. GenBank accession numbers were listed for the outgroup sequences.
3. Results and Discussion
We investigated the fungal diversity in Warren Cave though clone libraries. Soil substrate extraction was used to concentrate the fungal portion of the community prior to total DNA extraction. The habitat was highly oligotrophic with only 126 μg/g organic carbon (151 μg/g total carbon) and relatively moist with 50% soil moisture. Overall fungal diversity was moderate  with 266 fungal ITS clone sequences representing a total of 61 species. All were within the Ascomycota (Figure 2) and Basidiomycota (Figure 3) phyla, with no Chytridiomycota or Zygomycota represented. Near equal distribution of Ascomycota and Basidomycota taxa were represented in the Warren Cave clone libraries (31 Ascomycota/30 Basidomycota) unlike in nearby McMurdo Dry Valley habitats where Basidomycota dominate, especially in arid habitats [11,12,13]. The data in Table 1 show that a vast majority of clones found in Warren Cave can be identified to the species level (80%). Most of the remainder are relatively close matches with only one, a potential Malassezia species, with the closest match below 90% (82% identity with Malassezia sympodialis). The clones shown in this work are those that passed the criteria listed in the methods, yet within some of the chimeric clones (and not included in this analysis) DNA fragments of other organisms were found. These fragments were from organisms associated with humans. The most abundant of these were most closely identified as cabbage, soybeans, cereal grains and buckwheat. Interestingly, one of the dominant organisms found in the McMurdo Dry Valley soils, nematodes  were absent from these clone libraries, even in fragments.
Data on fungal communities in Antarctica still remain quite incomplete, however, it is possible to draw comparisons between our data from a Mt. Erebus DOVE to one other extreme environment in the McMurdo area, the nearby McMurdo Dry Valleys soils. The McMurdo Dry Valley soils are also highly oligotrophic, with some of the lowest organic carbon levels reported  and similar to those reported here. Their soil communities experience low temperature and rapid temperate swings, high UV radiation and desiccation , while the Mt. Erebus DOVEs have relatively moderate and constant temperature, no light, thus no UV radiation and a moist environment. In addition, many of the soils in the McMurdo Dry Valleys are basic with pH ranging up to pH10 , while this Warren Cave site was slightly acidic (pH 5.2). Therefore it is not surprising that the fungal communities are different. The typical number of fungal species found in any one soil community isolated from the McMurdo Dry Valleys is low, often below ten [11,12] whereas the fungal diversity found in Warren Cave was found to be much higher (61 species). The relative higher number of Ascomycota taxa found in Warren Cave compared with other studies in the McMurdo Dry Valleys may reflect the more stressful condition found in the latter. Yeast species in studies of the McMurdo Dry Valleys were dominated by basidiomycetous species (89%), most particularly those from the genus Cryptococcus (33%) . The dominance of Cryptococcus species in soil, particularly arid soil, has been ascribed to their ability to produce polysaccharide capsules . In contrast, only two Cryptococcus species were found in Warren Cave. Further, Glaciozyma watsonii has been isolated numerous times from soil from Continental Antarctic soil [12,18,19] and can be an abundant member of the McMurdo Dry Valley soil community, but are represented by only six clones (4.9%) in Warren Cave. Rhodotorula mucilaginosa has also been cultured from some of the most dry and cold locations in Antarctica, such as Sponsors Peak (03SP24) and a peak above Niebelungen Valley, in the Asgard Range (03NB35)  yet was represented by only 2 clones (1.6%) of the Warren Cave libraries.
Aureobasidium pullulans a yeast-like fungus, Aspergillus penicillioides and Alternaria alternata were found to be the dominating members of the Ascomycota (Figure 4a) from the Warren Cave fungal community. All of these species are cosmopolitan and have been isolated numerous times from the Antarctic . The most dominant Basidiomycota taxa found (Figure 4b) were Malassezia sp. (37% of the clones), yeasts most typically found associated with animals. Although Malassezia has also been identified from a clone library originating from McMurdo Dry Valleys desert soils of Taylor Valley, Antarctica (near a highly used pathway)  two of the species found in this study (M. globosa and M. restricta) are know to require lipids for growth and are common in human dandruff and seborrheic dermatitis . This high proportion of human associated yeasts represented in the Warren Cave clone libraries suggests human contamination of the site. The second most abundant taxa of the Basidomycota was a Peniophora species, a member of a genus most known for wood rot .
Although several fungal species found in Warren Cave are cosmopolitan, some have been shown to be capable of efficient colonization on minerals and sterile soil , abilities that enhance the probability that these organisms are active members of the DOVE community. For example Irpex lactecus, a white rot fungus, has been suggested as a potential bioremediation agent precisely because of its ability to utilize minerals and thrive in sterile soil. . Aureobasidium pullulans has been isolated often from Antarctica, including McMurdo Dry Valley soil and has been found on the inner part of the Chernobyl inner containment system . Both of these species may be early colonizers of oligotrophic habitats and potentially native Antarctic DOVE inhabitants.
The Warren Cave fungal community appears to have been influenced by humans. The cave has been visited throughout the years by both researchers and casual visitors. Evidence of human involvement in Warren Cave is supported by the findings of several Malassezia species. Finding species in a clone library alone does not necessary mean that they are active members of the community and more research will have to be carried out to determine their role, if any, in the Warren Cave soil community. As a result, it may not be surprising that Warren Cave is somewhat biologically compromised, and currently contains items that may impact and alter cave microbial communities (e.g., metal or bamboo stakes, instruments such as temperature recorders, batteries metal wires, etc.). It is clear that some of these practices profoundly impact the local microbial communities.
Even though Warren Cave has had human impact on its microbial community, other caves around the summit of Mt. Erebus remain untouched and therefore are potentially very valuable natural research laboratories for the study of DOVEs. The U.S. National Science Foundation has begun a procedure to develop a code of conduct for entering ice caves on Mt. Erebus. One of the first steps in this effort should be to determine which caves remain pristine and therefore are suitable candidates for microbial DOVE research.
Our data show that microbial communities in Mt. Erebus Ice Cave DOVEs contain diverse and specialized fungal communities that are likely to form a complex microbial foodweb that is independent from photosynthesis and primarily uses energy from chemolithotrophic metabolic processes. Very little is known about their function in these ecosystems, but several species are known to grow on mineral substrates in sterile soil supporting an active role. In addition, our study shows that a survey of fungi is a very sensitive indicator identifying the potential of human disturbance of these environments.
The authors would like to thank project co-PI Brad Tebo for insightful discussions and Rick Davis, Katherine Earle, Caleb Slemmons and Sarah Turner for their laboratory assistance, as well as Raytheon Polar Support Service, and PHI for logistical and laboratory support while in Antarctica. In addition, the authors give sincere thanks to the anonymous reviews for help in improving this manuscript. Funding was provided for this project by NSF Office of Polar Programs award #ANT-0739696 to the authors.
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