Cianofícies i algues aerofítiques de substrats carbonatats.

Atmophytic Cyanophyta and Algae from limestone substrata. The walls of caves and tombs support an abundant colonization of light-dependent organisms. A total of 4 liverworts, 3 mosses, 7 lichens and 28 cyanophyta and algae are reported from 3 collecting sites. The development and specific composition of these organisms is related to microclimatic parameters. Opportunistic species present in soils are found on the mouth of hypogeal niches. Light attenuation allows the development of calcifying cyanophyta following a succesional pattern, each level having a different dominant species. Communities dominated by Scytonema julianum are replaced by Herpyzonema pulverulentum and, towards the less iluminated area, by Geitleria calcarea and Loriella sp. Key words: Caves, Light attenuation, Non vascular plants, Colonization, Calcifying cyanophyta, Scytonema julianum, Herpyzonema pulverulentum, Geitleria calcarea, Chlorophyta, Diatoms, Microclimatic gradient.

Professor CREU CASAS i SICART (1913-2007)

Creu Casas i Sicart, Professor Emeritus at the Autonomous University of Barcelona, Catalonia, and a member of the Insti­tute of Catalan Studies (IEC) since 1978, died at the advanced yet still active age of 94 in Bellaterra on 20 May 2007, after a brief illness. She was unquestionably the most prominent bota­nist in the field of bryological research (mosses, liverworts, and hornworts) covering the entire Iberian Peninsula and Balearic Islands in the past 50 years. She also served as the president (1980-1982) of one of the most prestigious affiliates of our in­ stitute, the Catalan Institution of Natural History

Macrofossils in Raraku Lake (Easter Island) integrated with sedimentary and geochemical records towards a palaeoecological synthesis for the last 34,000 years

Macrofossil analysis of a composite 19 m long sediment core from Rano Raraku Lake (Easter Island)was related to litho-sedimentary and geochemical features of the sediment. Strong stratigraphical patterns are shown by indirect gradient analyses of the data. The good correspondence between the stratigraphical patterns derived from macrofossil (Correspondence Analysis) and sedimentary and geochemical data (Principal Component Analysis) shows that macrofossil associations provide sound palaeolimnological information in conjunction with sedimentary data. The main taphonomic factors in fluencing the macrofossil assemblages are run-off from the catchment, the littoral plant belt, and the depositional environment within the basin. Five main stages during the last 34,000 calibrated years BP (cal yr BP) are characterised from the lithological, geochemical, and macrofossil data. From 34 to 14.6 cal kyr BP (last glacial period) the sediments were largely derived from the catchment, indicating a high energy lake environment with much erosion and run-off bringing abundant plant trichomes, lichens, and mosses into the centre of Raraku Lake.

Els briòfits de les basses de l’Albera, Alt Empordà

We have studied some depressions and areas temporarily flooded where after the water evaporates, a high diversity and abundance of bryophyta can be observed on the emerged soil. For the distribution of these bryophytes we have established three concentric zones according to their humidity level. At the most external one, which is seldom flooded, the hepatics Riccia gougetiana and Fossombronia maritima were found, as well as various Anthocerotae. At the emerged zone Pseudephemerum nitidum, Archidium alternifolium and a high number of Riccia species, such as R. macrocarpa and R. warnstorfii could be found. In some depressions with a long flooding period, we observed pleurocarpous mosses such as Amblystegium riparium and Drepanocladus aduncus