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Ganoderma is a large, diverse and globally-distributed genus in the Basidiomycota that includes species causing a white rot form of wood decay on a variety of tree species. For the past century, many studies of Ganoderma in North America and other regions of the world have used the name G. lucidum sensu lato for any laccate (shiny or varnished) Ganoderma species growing on hardwood trees or substrates. Molecular studies have established that G. lucidum sensu stricto (Curtis) Karst is native to Europe and some parts of China. To determine the species of the laccate Ganoderma that are present in the United States, we studied over 500 collections from recently collected samples and herbarium specimens from hardwoods, conifers, and monocots. A multilocus phylogeny using ITS, tef1α, rpb1 and rpb2 revealed three well-supported clades, similar to previously reported findings. From the U.S. collections, thirteen taxa representing twelve species were identified, including: G. curtisii, G. lucidum sensu stricto, G. martinicense, G. oregonense, G. polychromum, G. ravenelii, G. sessile, G. tsugae, G. tuberculosum, G. cf. weberianum, G. zonatum, and Tomophagus colossus (syn. G. colossus). The species G. meredithiae is synonymized with G. curtisii, and considered a physiological variant that specializes in decay of pines. The designation G. curtisii f.sp. meredithiae forma specialis nov. is proposed. Species such as G. curtisii and G. sessile, once considered as G. lucidum sensu lato, were found to be divergent from one another, and highly divergent from G. lucidum sensu stricto. Morphological characteristics such as context tissue color and features (e.g. melanoid bands), basidiospore shape and size, geographic location, and host preference were found to aid in species identification. Surprisingly, G. lucidum sensu stricto was found in the U.S., but only in geographically restricted areas of northern Utah and California. These collections appear to have resulted from the introduction of this species into the United States possibly from mushroom growers producing G. lucidum outdoors. Overall, this study clarifies the chaotic taxonomy of the laccate Ganoderma in the United States, and will help to remove ambiguities from future studies focusing on the North American species of laccate Ganoderma. [ABSTRACT FROM AUTHOR]

Scientists working at New Harbor, Antarctica in November 1959 used a wooden crate as a makeshift workspace and kitchen. The structure has been used intermittently over the subsequent decades and still remains at the site with various materials left in and around it. The wooden structure was assessed for deterioration and samples collected to determine the diversity of fungi at the site after 43 years in the Antarctic environment. Results from these investigations are compared to the results from research on the historic huts of Ross Island, approximately 70 km east of New Harbor that were built 48-58 years earlier. Our analysis shows the wood of the New Harbor structure is extremely weathered and soft rot decay was detected in the wood in contact with the ground. Fungal cultures isolated from wood of the structure were identified using sequences of the internal transcribed spacer region of the rDNA. Several species of Cadophora were identified including C. malorum, C. luteo-olivacea, C. fastigiata and a previously undescribed species designated C. sp. NH. Laboratory decay experiments using two Cadophora species isolated from New Harbor demonstrated extensive decay and loss of biomass in hardwood wafers after 16 weeks. Other fungi isolated from the wood included species of Cladosporium, Hormonema, Penicillium and Lecythophora. Wind erosion has also severely affected the structure's exterior wood causing deep furrowing between earlywood and latewood cells. In general, the deterioration and fungi found at the site were similar to those found at the historic expedition huts on Ross Island, however, one species obtained is unique to the New Harbor site. This research expands our knowledge of the microbes colonizing wood brought into the polar environment and provides additional information on deterioration and decomposition processes occurring in Antarctica. [ABSTRACT FROM AUTHOR]