Tropical Bryology, Volume 25 (2004)
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Tortula flavinervis Dixon var. parviretis Sainsbury is Barbula crinita Schultz. The type of Phasconia balansae Müll. Hal. was not located, only a plate of the type material was seen. Phasconia balansae Müll. Hal. and Astomum platystegium Dixon are considered as identical. The occurrence of Weissia brachycarpa (Nees & Hornsch.) Jur. in Australia is doubtful. Comments on several nomina nuda are given. No material was located for Hymenostomum pertortile Müll. Hal. nom. nud. Weissia latiuscula Müll. Hal. is reported new for Australia.
A revised and updated literature-based checklist of Hawaiian mosses is presented. Geographic coverage includes the eight main Hawaiian Islands; the Northwestern Hawaiian Islands are excluded. The checklist is alphabetically ordered by scientific names; the family is noted for each genus. Synonyms and misapplied names are cross-referenced to the accepted names. A bibliography of supporting references is included.
En los diferentes tipos de paisaje del corregimiento de Tarapacá (Amazonas-Colombia) se estudió la distribución vertical de los briófitos sobre los forofítos, encontrándose que alrededor del 41% de las especies son exclusivas del dosel y el 35% exclusivas del sotobosque. Además, se analiza la selectividad de las especies de briófitos por diferentes tipos de hábitats (base de tronco, corteza baja, corteza alta, ramas bajas, ramas altas, epífilos, roca, hojarasca, suelo y troncos caídos en descomposición) y sus formas de crecimiento. En todos los tipos de paisaje, la selectividad de la brioflora fue mayor sobre la corteza baja de los árboles y los hábitats del dosel (hojas y ramas del dosel a más de 18 m de altura sobre el suelo), con las formas de crecimiento más comunes (felpas lisas, felpas rugosas e hilos) y el mayor número de especies (especialistas y/o generalistas). Los resultados obtenidos para Tarapacá, fueron comparados con otras regiones similares.
New and remarkable records of bryophytes from Venezuela, Brazil, Costa Rica and Ecuador are reported. Diphyscium chiapense and Hedwigia ciliata var. leucophaea are new to South America. New to Venezuela are Grimmia reflexidens, Metzgeria claviflora, Pilopogon peruvianus and Racomitrium subsecundum; Grimmia navicularis and G. trichophylla are firstly reported for Brazil; Aphanolejeunea microscopica var. africana, A. minuta, A. sintenisii, Cololejeunea bischleriana, Metalejeunea cucullata, and Hyophila nymaniana represent new records for Costa Rica, and new to Ecuador are Diphyscium longifolium, Erpodium beccarii, Macrocolura sagittistipula, and (for continental Ecuador) Marchantia berteroana. Further new records to the states of that countries and rarely collected species are listed. All specimens are deposited in the private herbaria of the authors, duplicates in different herbaria as indicated.
New records are presented based on a collection of Campylopus specimens made by the second author in the Western Cape Province of South Africa. The austral species Campylopus clavatus (R. Brown) Wils. in Hook. and Campylopus vesticaulis Mitt. are reported for the first time for Africa, and Campylopus acuminatus Mitt. var. kirkii (Mitt.) J.-P. Frahm is recorded for the second time for Africa. Campylopus arctocarpus (Hornsch.) Mitt. ssp. madegassus (Besch.) J.-P. Frahm is reported for the first time for the Republic of South Africa, and this is the southernmost record of this species. Campylopus simii Schelpe is not synonymous with C. julaceus Jaeg. ssp. arbogastii (Ren. & Card.) J.-P. Frahm but combined here as new as a variety of C. pilifer Brid.
Two epiphyllous Lejeuneaceae, Cololejeunea surinamensis and Drepanolejeunea polyrhiza, previously known from Amazonian Brazil, are recorded for the first time in Colombia. They were found as epiphylls on understory shrubs in the middle Caquetá area in Colombian Amazonia. Cololejeunea surinamensis was found in the Tierra Firme forests and D. polyrhiza was found in the floodplains of the Caquetá River.
We investigated patterns of bryophyte species richness and composition in two forest types of Colombian Amazonia, non-flooded tierra firme forest and floodplain forest of the Caquetá River. A total of 109 bryophyte species were recorded from 14 0.2 ha plots. Bryophyte life forms and habitats were analyzed, including the canopy and epiphylls. Bryophyte species did not show significant differences between landscapes but mosses and liverworts were different and with opposite responses balancing the overall richness. Independence test showed differences in both life form and habitat use distribution between the two forest types with more fan and mat bryophytes species in the floodplains, and more epiphytic liverworts in the tierra firme forest. Correspondence analysis showed differences in the bryophyte species assemblage between the two forest types where they may be responding to the higher humidity provided by the flooding. Despite of, the environmental differences detected, epiphyll species assemblages were not strongly affected. Apparently, epiphyll habitat is stressful enough to hide the environmental differences between the flooded and Tierra firme forests.
Los fósiles atribuidos a briófitos son escasos, principalmente en rocas paleozoicas a pesar de ser registrados desde el Silúrico. Para la División Bryophyta, los fósiles correspondientes a la Clase Bryopsida comienzan a ser encontrados a partir del Carbonífero, aunque son bastante escasos. Registros más abundantes son conocidos para el Pérmico en rocas de las cuencas de Petchora, Kuznetsk y en la Plataforma Rusa, así como en la Antártica, en la Cuenca del Karoo (África del Sur) e India. Especímenes de gametófitos con esporofitos pleurocárpicos del género Dwykea fueron colectados en los niveles inferiores del Subgrupo Itararé, próximos a la ciudad de Campinas, Estado de S. Paulo. Estos fósiles corresponden al primer registro para el periodo Carbonífero de gametofitos femeninos fértiles. La microflora asociada a los fósiles de Dwykea permite establecer correlaciones con la Palinozona Ahrensisporites cristatus de edad westfaliana. Además los niveles donde fueron colectados los ejemplares de Dwykea corresponden a sedimentos proglaciales, que son interpretados como una vegetación de tundra que habitaba en el margen noreste de la Cuenca del Paraná, durante el Westfaliano.