A World Review of Fungi, Yeasts, and Slime Molds in Caves Karen J
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First Record of the Genus Ilyomyces for North America, Parasitizing Stenus Clavicornis
Bulletin of Insectology 66 (2): 269-272, 2013 ISSN 1721-8861 First record of the genus Ilyomyces for North America, parasitizing Stenus clavicornis Danny HAELEWATERS Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, USA Abstract The ectoparasitic fungus Ilyomyces cf. mairei (Ascomycota Laboulbeniales) is reported for the first time outside Europe on the rove beetle Stenus clavicornis (Coleoptera Staphylinidae). This record is the first for the genus Ilyomyces in North America. De- scription, illustrations, and discussion in relation to the different species in the genus are given. Key words: ectoparasites, François Picard, Ilyomyces, rove beetles, Stenus. Introduction 1939) described Acallomyces lavagnei F. Picard (Picard, 1913), which he later reassigned to a new genus Ilyomy- Fungal diversity is under-documented, with diversity ces while adding a second species, Ilyomyces mairei F. estimates often based only on relationships with plants. Picard (Picard, 1917). For a long time both species were Meanwhile, the estimated number of fungi associated only known from France, until Santamaría (1992) re- with insects ranges from 10,000 to 50,000, most of ported I. mairei from Spain. Weir (1995) added two which still need be described from the unexplored moist more species to the genus: Ilyomyces dianoi A. Weir and tropical regions (Weir and Hammond, 1997). Despite Ilyomyces victoriae A. Weir, parasitic on Steninae from the biological and ecological importance the relation- Sulawesi, Indonesia. This paper presents the first record ship might have for studies of co-evolution of host and of Ilyomyces for the New World. parasite and in applications in biological control, insect- parasites have received little attention, unfortunately. -
The Coume Ouarnède System, a Hotspot of Subterranean Biodiversity in Pyrenees (France)
diversity Article The Coume Ouarnède System, a Hotspot of Subterranean Biodiversity in Pyrenees (France) Arnaud Faille 1,* and Louis Deharveng 2 1 Department of Entomology, State Museum of Natural History, 70191 Stuttgart, Germany 2 Institut de Systématique, Évolution, Biodiversité (ISYEB), UMR7205, CNRS, Muséum National d’Histoire Naturelle, Sorbonne Université, EPHE, 75005 Paris, France; [email protected] * Correspondence: [email protected] Abstract: Located in Northern Pyrenees, in the Arbas massif, France, the system of the Coume Ouarnède, also known as Réseau Félix Trombe—Henne Morte, is the longest and the most complex cave system of France. The system, developed in massive Mesozoic limestone, has two distinct resur- gences. Despite relatively limited sampling, its subterranean fauna is rich, composed of a number of local endemics, terrestrial as well as aquatic, including two remarkable relictual species, Arbasus cae- cus (Simon, 1911) and Tritomurus falcifer Cassagnau, 1958. With 38 stygobiotic and troglobiotic species recorded so far, the Coume Ouarnède system is the second richest subterranean hotspot in France and the first one in Pyrenees. This species richness is, however, expected to increase because several taxonomic groups, like Ostracoda, as well as important subterranean habitats, like MSS (“Milieu Souterrain Superficiel”), have not been considered so far in inventories. Similar levels of subterranean biodiversity are expected to occur in less-sampled karsts of central and western Pyrenees. Keywords: troglobionts; stygobionts; cave fauna Citation: Faille, A.; Deharveng, L. The Coume Ouarnède System, a Hotspot of Subterranean Biodiversity in Pyrenees (France). Diversity 2021, 1. Introduction 13 , 419. https://doi.org/10.3390/ Stretching at the border between France and Spain, the Pyrenees are known as one d13090419 of the subterranean hotspots of the world [1]. -
THE PROBLEM of LAMPENFLORA in SHOW CAVES – Arrigo A
ANDYSEZ 56 LAMPENFLORA YET AGAIN! Thus Lampenflora Part 4 – Andy Spate The very distinguished and knowledgeable results for lampenflora growth control were very Professor Arrigo Cigna has contributed a great promising. This procedure is especially useful deal to our understanding of cave environments when applied to actively growing lampenflora. particularly in relation to radon, carbon dioxide, Once lampenflora is covered with flowstone, the cave environmental monitoring – and to the oxidizing effect of H2O2 is drastically reduced lampenflora problem. Below you will find a recent [as with hypochlorite]. presentation from Arrigo given at the ISCA Congress in Slovakia in October 2010 (Cigna in So what is meant by buffering and why and how press, 2010). do we do it? Many of us have tried to re-invent the wheel Faimon’s et al (2003) details extensive and in- playing about with concentrations of sodium depth research on the use of hydrogen peroxide hypochlorite and calcium hypochlorite in spite of for lampenflora control. Unlike hypochlorite, the admonishments of Tom Aley, for example, peroxide can erode calcite – not much, but some. who has very fixed views on 5.25% hypochlorite (Aley and Aley 1992). Adding some of your local limestone or calcite to the peroxide solution for a few hours or overnight We have discussed other chemicals including reduces or halts this issue. It just adds to the potent biocides, altering light frequencies and the more complex approach of using peroxide rather use of ultraviolet light in earlier ANDYSEZs than hypochlorite. (Numbers 48, 49 & 50 – look on your ACKMA CD ROM). All of these have drawbacks and some – The disadvantages include: such as the use of hypochlorite – may have very considerable impacts on cave environments – • The need to buffer the peroxide solution; especially their biota. -
Studies of the Laboulbeniomycetes: Diversity, Evolution, and Patterns of Speciation
Studies of the Laboulbeniomycetes: Diversity, Evolution, and Patterns of Speciation The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:40049989 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA ! STUDIES OF THE LABOULBENIOMYCETES: DIVERSITY, EVOLUTION, AND PATTERNS OF SPECIATION A dissertation presented by DANNY HAELEWATERS to THE DEPARTMENT OF ORGANISMIC AND EVOLUTIONARY BIOLOGY in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of Biology HARVARD UNIVERSITY Cambridge, Massachusetts April 2018 ! ! © 2018 – Danny Haelewaters All rights reserved. ! ! Dissertation Advisor: Professor Donald H. Pfister Danny Haelewaters STUDIES OF THE LABOULBENIOMYCETES: DIVERSITY, EVOLUTION, AND PATTERNS OF SPECIATION ABSTRACT CHAPTER 1: Laboulbeniales is one of the most morphologically and ecologically distinct orders of Ascomycota. These microscopic fungi are characterized by an ectoparasitic lifestyle on arthropods, determinate growth, lack of asexual state, high species richness and intractability to culture. DNA extraction and PCR amplification have proven difficult for multiple reasons. DNA isolation techniques and commercially available kits are tested enabling efficient and rapid genetic analysis of Laboulbeniales fungi. Success rates for the different techniques on different taxa are presented and discussed in the light of difficulties with micromanipulation, preservation techniques and negative results. CHAPTER 2: The class Laboulbeniomycetes comprises biotrophic parasites associated with arthropods and fungi. -
Phylogeny of the Genus Arachnomyces and Its Anamorphs and the Establishment of Arachnomycetales, a New Eurotiomycete Order in the Ascomycota
STUDIES IN MYCOLOGY 47: 131-139, 2002 Phylogeny of the genus Arachnomyces and its anamorphs and the establishment of Arachnomycetales, a new eurotiomycete order in the Ascomycota 1, 2 1* 3 2 C. F. C. Gibas , L. Sigler , R. C. Summerbell and R. S. Currah 1University of Alberta Microfungus Collection and Herbarium, Edmonton, Alberta, Canada; 2Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada; 3Centraalbureau voor Schimmelcultures, Utrecht, The Netherlands Abstract: Arachnomyces is a genus of cleistothecial ascomycetes that has morphological similarities to the Onygenaceae and the Gymnoascaceae but is not accommodated well in either taxon. The phylogeny of the genus and its related anamorphs was studied using nuclear SSU rDNA gene sequences. Partial sequences were determined from ex-type cultures representing A. minimus, A. nodosetosus (anamorph Onychocola canadensis), A. kanei (anamorph O. kanei) and A. gracilis (anamorph Malbranchea sp.) and aligned together with published sequences of onygenalean and other ascomycetes. Phylogenetic analysis based on maximum parsimony showed that Arachnomyces is monophyletic, that it includes the hyphomycete Malbranchea sclerotica, and it forms a distinct lineage within the Eurotiomycetes. Based on molecular and morphological data, we propose the new order Arachnomycetales and a new family Arachnomycetaceae. All known anamorphs in this lineage are arthroconidial and have been placed either in Onychocola (A. nodosetosus, A. kanei) or in Malbranchea (A. gracilis). Onychocola is considered appropriate for disposition of the arthroconidial states of Arachnomyces and thus Malbranchea sclerotica and the unnamed anamorph of A. gracilis are redisposed as Onychocola sclerotica comb. nov. and O. gracilis sp. nov. Keywords: Eurotiomycetes, Arachnomycetales, Arachnomycetaceae, Arachnomyces, Onychocola, Malbranchea sclerotica, SSU rDNA, Ascomycota, phylogeny Introduction described from herbivore dung maintained in damp chambers (Singh & Mukerji, 1978; Mukerji, pers. -
Position Specificity in the Genus Coreomyces (Laboulbeniomycetes, Ascomycota)
VOLUME 1 JUNE 2018 Fungal Systematics and Evolution PAGES 217–228 doi.org/10.3114/fuse.2018.01.09 Position specificity in the genus Coreomyces (Laboulbeniomycetes, Ascomycota) H. Sundberg1*, Å. Kruys2, J. Bergsten3, S. Ekman2 1Systematic Biology, Department of Organismal Biology, Evolutionary Biology Centre, Uppsala University, Uppsala, Sweden 2Museum of Evolution, Uppsala University, Uppsala, Sweden 3Department of Zoology, Swedish Museum of Natural History, Stockholm, Sweden *Corresponding author: [email protected] Key words: Abstract: To study position specificity in the insect-parasitic fungal genus Coreomyces (Laboulbeniaceae, Laboulbeniales), Corixidae we sampled corixid hosts (Corixidae, Heteroptera) in southern Scandinavia. We detected Coreomyces thalli in five different DNA positions on the hosts. Thalli from the various positions grouped in four distinct clusters in the resulting gene trees, distinctly Fungi so in the ITS and LSU of the nuclear ribosomal DNA, less so in the SSU of the nuclear ribosomal DNA and the mitochondrial host-specificity ribosomal DNA. Thalli from the left side of abdomen grouped in a single cluster, and so did thalli from the ventral right side. insect Thalli in the mid-ventral position turned out to be a mix of three clades, while thalli growing dorsally grouped with thalli from phylogeny the left and right abdominal clades. The mid-ventral and dorsal positions were found in male hosts only. The position on the left hemelytron was shared by members from two sister clades. Statistical analyses demonstrate a significant positive correlation between clade and position on the host, but also a weak correlation between host sex and clade membership. These results indicate that sex-of-host specificity may be a non-existent extreme in a continuum, where instead weak preferences for one host sex may turn out to be frequent. -
Laboulbeniomycetes, Eni... Historyâ
Laboulbeniomycetes, Enigmatic Fungi With a Turbulent Taxonomic History☆ Danny Haelewaters, Purdue University, West Lafayette, IN, United States; Ghent University, Ghent, Belgium; Universidad Autónoma ̌ de Chiriquí, David, Panama; and University of South Bohemia, Ceské Budejovice,̌ Czech Republic Michał Gorczak, University of Warsaw, Warszawa, Poland Patricia Kaishian, Purdue University, West Lafayette, IN, United States and State University of New York, Syracuse, NY, United States André De Kesel, Meise Botanic Garden, Meise, Belgium Meredith Blackwell, Louisiana State University, Baton Rouge, LA, United States and University of South Carolina, Columbia, SC, United States r 2021 Elsevier Inc. All rights reserved. From Roland Thaxter to the Present: Synergy Among Mycologists, Entomologists, Parasitologists Laboulbeniales were discovered in the middle of the 19th century, rather late in mycological history (Anonymous, 1849; Rouget, 1850; Robin, 1852, 1853; Mayr, 1853). After their discovery and eventually their recognition as fungi, occasional reports increased species numbers and broadened host ranges and geographical distributions; however, it was not until the fundamental work of Thaxter (1896, 1908, 1924, 1926, 1931), who made numerous collections but also acquired infected insects from correspondents, that the Laboulbeniales became better known among mycologists and entomologists. Thaxter set the stage for progress by describing a remarkable number of taxa: 103 genera and 1260 species. Fewer than 25 species of Pyxidiophora in the Pyxidiophorales are known. Many have been collected rarely, often described from single collections and never encountered again. They probably are more common and diverse than known collections indicate, but their rapid development in hidden habitats and difficulty of cultivation make species of Pyxidiophora easily overlooked and, thus, underreported (Blackwell and Malloch, 1989a,b; Malloch and Blackwell, 1993; Jacobs et al., 2005; Gams and Arnold, 2007). -
Laboulbeniales (Ascomycota) of the Canary Islands
VIERAEA Vol. 32 107-115 Santa Cruz de Tenerife, diciembre 2004 ISSN 0210-945X Laboulbeniales (Ascomycota) of the Canary Islands ERIK ARNDT * & SERGI SANTAMARÍA** *Anhalt University of Applied Sciences, Department LOEL, Strenzfelder Allee 28, D-06406 Bernburg, Germany. Correspondence address. *Unitat de Botànica, Departament de Biologia Animal, de Biologia Vegetal i d’Ecologia, Facultat de Ciències Universitat Autònoma de Barcelona, E-08193-Bellaterra (Barcelona), SPAIN ARNDT, E. & S. SANTAMARÍA (2004). Laboulbeniales (Ascomycota) de las islas Canarias. VIERAEA 32: 107-115. RESUMEN: Se presenta una lista con 23 especies y 8 géneros de Laboulbeniales (Ascomycota). Seis de ellas son primeras citas para las islas Canarias. La mayoría de las especies citadas infectan Carabidae (Coleoptera). Muchas de las especies de hospedantes (23) son endémicas, siendo sólo nueve las de hospedantes que también se encuentran fuera de la región Macaronésica. Los Carabidae, como familia más diversa de hospedantes, incluyen 21 especies endémicas y 6 de amplia distribución. Las pautas de distribución de Laboulbeniales dependen de dos factores ecológicos (humedad y biodiversidad de los hospedantes) que varían mucho entre las distintas islas. Palabras clave: Laboulbeniales, Carabidae, Staphylinidae, Anthicidae, Blattaria, Ephydridae, islas Canarias. ABSTRACT: The list includes 23 species of Laboulbeniales (Ascomycota) in 8 genera. Six species are new for the Canary Islands. The majority of recorded species infests Carabidae (Coleoptera). Most host species (23) are endemic, only nine hosts also occur outside the Macaronesian region. There are 21 endemic and 6 widespread host species in the Carabidae as most diverse host family. The distribution pattern of Laboulbeniales corresponds with two ecological factors (moisture and host biodiversity respectively) which vary strongly between the different islands. -
Caves of Aggtelek Karst and Slovak Karst Hungary & Slovakia
CAVES OF AGGTELEK KARST AND SLOVAK KARST HUNGARY & SLOVAKIA The variety and concentration of their formations make these cave systems of 712 caves excellent representatives of a temperate-zone karstic network. They also display an extremely rare combination of tropical and glacial climatic effects, making it possible to study geological history over tens of millions of years. COUNTRY Hungary and Slovakia NAME Caves of Aggtelek Karst and Slovak Karst NATURAL WORLD HERITAGE TRANSBOUNDARY SERIAL SITE 1995: The cave systems of the two protected areas jointly inscribed on the World Heritage List under Natural Criterion viii. 2000: Extended to include Dobšinská cave in Slovakia (660 ha). 2008: Extended by 87.8 ha. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] INTERNATIONAL DESIGNATIONS 1977: Slovensky Kras Protected Landscape Area designated a Biosphere Reserve under the UNESCO Man & Biosphere Programme (36,166 ha). 1979: Aggtelek National Park designated a Biosphere Reserve under the UNESCO Man & Biosphere Programme (19,247 ha); 2001: Baradla Cave System & Related Wetlands, Hungary (2,075 ha) and Domica Wetland in the Slovensky Kras, Slovak Republic (627 ha) both in Aggtelek National Park, designated a transboundary Wetland of International Importance under the Ramsar Convention. IUCN MANAGEMENT CATEGORY II National Parks BIOGEOGRAPHICAL PROVINCE Middle European Forest (2.11.5) GEOGRAPHICAL LOCATION Straddles the Slovensky Kras foothills of the Carpathian mountains on the border of southern Slovakia and northern Hungary 152 km northeast -
Coprophilous Fungal Community of Wild Rabbit in a Park of a Hospital (Chile): a Taxonomic Approach
Boletín Micológico Vol. 21 : 1 - 17 2006 COPROPHILOUS FUNGAL COMMUNITY OF WILD RABBIT IN A PARK OF A HOSPITAL (CHILE): A TAXONOMIC APPROACH (Comunidades fúngicas coprófilas de conejos silvestres en un parque de un Hospital (Chile): un enfoque taxonómico) Eduardo Piontelli, L, Rodrigo Cruz, C & M. Alicia Toro .S.M. Universidad de Valparaíso, Escuela de Medicina Cátedra de micología, Casilla 92 V Valparaíso, Chile. e-mail <eduardo.piontelli@ uv.cl > Key words: Coprophilous microfungi,wild rabbit, hospital zone, Chile. Palabras clave: Microhongos coprófilos, conejos silvestres, zona de hospital, Chile ABSTRACT RESUMEN During year 2005-through 2006 a study on copro- Durante los años 2005-2006 se efectuó un estudio philous fungal communities present in wild rabbit dung de las comunidades fúngicas coprófilos en excementos de was carried out in the park of a regional hospital (V conejos silvestres en un parque de un hospital regional Region, Chile), 21 samples in seven months under two (V Región, Chile), colectándose 21 muestras en 7 meses seasonable periods (cold and warm) being collected. en 2 períodos estacionales (fríos y cálidos). Un total de Sixty species and 44 genera as a total were recorded in 60 especies y 44 géneros fueron detectados en el período the sampling period, 46 species in warm periods and 39 de muestreo, 46 especies en los períodos cálidos y 39 en in the cold ones. Major groups were arranged as follows: los fríos. La distribución de los grandes grupos fue: Zygomycota (11,6 %), Ascomycota (50 %), associated Zygomycota(11,6 %), Ascomycota (50 %), géneros mitos- mitosporic genera (36,8 %) and Basidiomycota (1,6 %). -
Downloaded 10/01/21 04:52 AM UTC IAGA-REPORT 2007–2010 159
Acta Geod. Geoph. Hung., Vol. 46(2), pp. 158–214 (2011) DOI: 10.1556/AGeod.46.2011.2.4 HUNGARIAN NATIONAL REPORT ON IAGA 2007–2010 LSzarkaand GSatori´ Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences, POB 5, H-9401 Sopron, Hungary, e-mail: [email protected] This report is a collection of institutional and individual reports, edited by the Hungarian national delegates (L Szarka: 2007–2010 and G S´atori: 2010). In the reference lists the readers find papers published mainly between 2007 and 2010 in various geophysical journals (including journals edited in Hungary as Acta Geodaetica et Geophysica Hungarica, Geophysical Transactions, Magyar Geofizika, F¨oldtani K¨ozl¨ony,etc.). The major IAGA-related conferences in Hungary between 2007–2010 were as follows: the IAGA XI. Scientific Assembly (Sopron, 2009) as the most remarkable event of geo-science in Hungary, in that year; the VERSIM Workshop (Tihany, 2008), as an other international meeting; Ionosphere and Magnetosphere Seminars (Budapest, 2008; Baja, 2010); Inversion Workshop (Miskolc, 2008); annual meetings of the Association of Hungarian Geophysicists; annual meetings of Young Geologists and Geophysicists. The structure of this report follows more or less the structure of Hungarian activities in frames of IAGA. The numbering of sections (I–V) indicates the number of IAGA divisions, but the individual sections does not follow exactly the structure of IAGA working groups. Instead, each of the sections is divided into several subsections, corresponding to the related Hungarian results. Several scientific results are described in Section V, under the observatory de- scriptions, where activities of two Hungarian geo-electromagnetic observatories: Nagycenk and Tihany are summarized. -
Water Regime: Physical Features of the Site
Ramsar Site: 1092 – Baradla Cave System Ramsar Information Sheet May 2014 Additional information Water Regime: 1. Ground waters 1.1. Karstic water As the the Domica-Baradla Cave System is in a karstic region, the major part of the groundwater is stored in the tectonic fissures, fractures and dissolutional cavities of the karstified Triassic limestones and dolomites. The recharge derives from the rainfall infiltrating through the surface, and from meteoric waters flowing into the karst system through sinkholes. 1.2. Confined groundwater In the Domica-Baradla Cave System area confined groundwater occurs only south from Aggtelek, in the 50-100 m thick Pannonian clayey-sandy-pebbly sediments. This sequence is considered more or less impervious because of its clay content, therefore only 5% of the rainfall can infiltrate. A part of the infiltrating water feeds the karst beneath, another part flows laterally towards the springs on the south. Some local springs discharge on the surface of the clayey pebble horizons. 1.3. Unconfined groundwater Unconfined groundwater occurs only in the valleys of major streams, and in the fluvial pebbly sediments of basins. 2. Springs Springs can be best characterised by discharge, which is determined by the geological-morphological build-up of the catchment area, and basically by climatic conditions (rainfall, evaporation, melting). Depending on these conditions, the discharge of a spring may vary between a few l/min and a few thousand l/min. In this area the Jósva spring has the biggest discharge with a minimum of 3900 l/min and a maximum of 450.000 l/min (and 1.200.000 l/min in 1959).