Late Holocene vegetation, fire, climate and upper forest line dynamics in the Podocarpus National Park, southeastern Ecuador

Late Holocene vegetation, fire, climate and upper forest line dynamics were studied based on detailed pollen and charcoal analyses. Two sediment cores, from the Rabadilla de Vaca mire (RVM) and the Valle Pequeo bog (VP), with an age of about 2100 and 1630 cal yrs b.p., respectively, were taken at the modern upper forest line in the Parque Nacional Podocarpus (Podocarpus National Park) in southeastern Ecuador. The two pollen records reflect relatively stable vegetation with slight changes in floral composition during the recorded period. Changes of the proportion between subparamo and paramo vegetation are related to lower and higher frequency of fires. The RVM records show that the upper forest line moved to a higher elevation between 1630 and 880 cal yrs b.p., stabilising after 310 cal yrs b.p. Human impact is suggested by a high fire frequency, mainly between 1800-1600 and 880-310 cal yrs b.p. The VP records indicate no marked changes in the upper forest line. The charcoal records suggest an increased human impact from 230 cal yrs b.p. to the present. The results indicate that high fire frequency is an important factor in reducing the expansion of subparamo vegetation and upper montane rainforest and in favouring the distribution of grass paramo. Since there is a clear correlation between fire and vegetation dynamics, it is difficult to detect how far climate change also played a significant role in upper forest line changes during the late Holocene

AFFINITY AMONG MOUNTAIN-RANGES IN MEGAMEXICO - A PHYTOGEOGRAPHICAL SCENARIO

The concept of Megamexico as a phytogeographic unit has been introduced by Rzedowski (1991) on the basis of distribution patterns of genera. Until now precise information on the resemblance between plant communities in the proposed Megamexico was scarce. This phytosociological study documents the affinities between plant communities within Megamexico, based on studies from mountain ranges in Mexico (Sierra Chichinautzin, Sierra Nevada) and Guatemalan mountain ranges (Sierra de los Cuchumatanes, Cadena Volcanica). Data, collected in the style of Braun-Blanquet during extensive fieldwork, were pooled into a single data set, and analyzed by using (1) TWINSPAN, for plant community classification, (2) ordination (DCA), (3) alpha log series biodiversity-index to measure intergroup diversity, and (4) information on the altitudinal distribution of the vegetation belts. Classification showed that four communities were common to the two groups of mountain ranges, namely, alpine bunchgrassland, pine forest, fir forest and mixed forest. Along the altitudinal gradient Mexican communities are distributed 200 m higher than their Guatemalan equivalents. This appears to be an illustration of the 'Massenerhebungseffekt'. DCA showed that the first axis represents a set of minor differences of closely related ecological factors (e.g., temperature, precipitation) and the second a humidity gradient. The biodiversity index showed that the Mexican mixed forest was significantly more diverse than the Guatemalan mixed forest. From the present results, ecological conditions among mountain ranges in Megamexico differed significantly. To conclude, phytogeographical units in Megamexico can better be defined on basis of both historical and ecological characteristics of the communities

HIGH-ELEVATION CONIFEROUS VEGETATION OF GUATEMALA - A PHYTOSOCIOLOGICAL APPROACH

A phytosociological study of the juniper (locally called huito), pine (locally called sacch), pine-alder and fir forests of the Sierra de los Cuchumatanes and Cadena Volcanica in Guatemala was carried out. The Zurich-Montpellier approach was followed. In total 119 releves were sampled and the data were organised in phytosociological tables to distinguish vegetation clusters. TWINSPAN was used to evaluate major differences among plant communities. Seven zonal plant communities were distinguished and described, namely: (1) Relbunium microphyllum-Agrostis tolucensis, (2) Werneria nubigena-Agrostis exserta, (3) Lachemilla vulcania-Pinus hartwegii, (4) Holodiscus argenteus-Pinus hartwegii, (5) Hypnum cypressiforme-Juniperus standleyi, (6) Agave hurtei-Alnus firmifolia and (7) Sabazia pinetorum-Abies guatemalensis. This paper provides a thorough floristic characterisation of each community and outlines the major anthropogenic activities. To conclude, ecologic and floristic (dis)similarities between plant communities of the study area and those of Central Mexico, like the different altitudinal distribution of fir forests and the establishment of mid-successional communities such as the Agave hurteri-Alnus firmifolia were discussed

Chloroplast DNA Microsatellites Reveal Contrasting Phylogeographic Structure in Mahogany (Swietenia macrophylla King, Meliaceae) from Amazonia and Central America

Big-leaf mahogany (Swietenia macrophylla) is one of the most valuable and overharvested timber trees of tropical America. A description of the organization of genetic variation across its broad range would be useful for management of genetic diversity and for understanding its demographic history. Here we report on a phylogeographic analysis of mahogany based on six polymorphic cpDNA simple sequence repeat loci (cpSSRs) genotyped in 16 populations distributed across the Brazilian Amazon and Mesoamerica (N = 245 individuals). Of the 31 cpDNA haplotypes identified, 15 occurred in Amazonia and 16 in Mesoamerica with no single haplotype shared between the two regions. The populations from Central America showed moderate differentiation (FST = 0.36) while within population genetic diversity was generally high (mean Nei's HE = 0.639). In contrast, the Amazonian populations were strongly differentiated (FST = 0.95) and contained low haplotype diversity (mean HE = 0.176), with the exception of the highly diverse Marajoara population from the Eastern Amazon (HE = 0.925). SAMOVA identified a single Mesoamerican phylogroup and four Amazonian phylogroups, indicating stronger phylogeographic structure within Amazonia. The results demonstrate high levels of cpDNA variation and differentiation of regional S. macrophylla populations, and provide the first evidence of a major phylogeographic break between Mesoamerican and South American mahogany populations