56 PARALLEL SESSION | H III | TROPICAL AQUATIC ECOSYSTEMSPARALLEL SESSION | H III | TROPICAL AQUATIC ECOSYSTEMS 57TUESDAY 12:15 Hall H IIIOur first measurements of enhanced methane concentrations of 2 to 4μl L-1in air samples collected 10cm above the soil surface indicate a significantmethane emission from the swamp area. They also indicated a high spatialvariability of methane emission. The current knowledge suggest that palmswamps in western Amazonia are a tropical hotspot <strong>for</strong> soil C sequestration andthey may also be a significant methane source at the local, regional and globalperspective.LEAF FUNCTIONAL TRAITS OF AMAZONIAN FLOODPLAIN TREES INRELATION TO FLOODINGPia Parolin 11University of Hamburg, Hamburg, DE, pparolin@botanik.uni-hamburg.de1000 highly flooding tolerant tree species grow in Amazonian floodplain<strong>for</strong>ests. Growth, productivity and morphological adaptations are adjusted togradients of flooding intensity and nutrient availability. Plant physiology andmorphology are adapted to conditions in specific sites, and thus tree species arenot equally distributed, but <strong>for</strong>m a clear zonation along the flooding gradient.The main hypothesis of this talk is that leaves, which are among the mostimportant organs of a plant, reflect the differences in their morphoanatomicalstructures and show different adaptations and functional traits dependingon the environment the plant typically occurs in. However, results show thatthe relationship of leaf functional traits with flooding intensity and nutrientavailability are neglectable and – contrary to the expectations – no patternscould be detected. There are equal leaf adaptations in high and low positionsalong the flooding gradient, and in nutrient-poor and –rich environments. Thedifferences can be explained almost exclusively by the morphoanatomicalcharacteristics of pioneer trees which occur only in várzea.TUESDAY 12:30 Hall H IIIgtö<strong>Society</strong> <strong>for</strong> <strong>Tropical</strong> <strong>Ecology</strong> | Gesellschaft für Tropenökologie e.V. Status and future of tropical biodiversity | Frankfurt, 21 - 24 February 2011gtö
58 PARALLEL SESSION | H IV | RAIN FOREST STRUCTURE & DYNAMICSPARALLEL SESSION | H IV | RAIN FOREST STRUCTURE & DYNAMICS 59PARALLEL SESSION TUESDAY, HALL H IV:RAINFOREST STRUCTURE & DYNAMICSChair: Jürgen HomeierTHE TROPICAL LOWLAND CLOUD FOREST: A LOWLAND FORESTWITH MONTANE EPIPHYTE RICHNESSChristine Gehrig-Downie 1 , Andre Obregon 2 , Jörg Bendix 2 , S. RobbertGradstein 31University of Göttingen, Goettingen, DE, cgehrig@gwdg.de, 2 University of Marburg,Marburg, DE, 3 Muséum National d’Histoire Naturelle, Paris, FRTUESDAY 11:15 Hall H IVTHE STRUCTURE OF TROPICAL RAINFORESTS: WHAT CAN WE LEARNFROM TREE SIZE DISTRIBUTIONS?Franziska Taubert 1 , Hans-Jürgen Dobner 2 , Andreas Huth 11 Helmholtz-Centre UFZ, Leipzig, DE, franziska.taubert@ufz.de, 2 HTWK Leipzig -University of Applied Science, Leipzig, DEIn the global discussion on climate change and environmental protection tropicalrain<strong>for</strong>ests take up an important position. Their high biomass and biodiversityis closely related to their structure and dynamics. <strong>Tropical</strong> rain<strong>for</strong>ests showa high variety in canopy structure. Local variations in <strong>for</strong>est biomass can be tracedback to variations in tree sizes. Investigations on the stem size distributionof tropical rain<strong>for</strong>ests are important <strong>for</strong> the estimation of <strong>for</strong>est biomass andthus, the role of these <strong>for</strong>ests in the carbon cycle.The novel <strong>for</strong>est type “<strong>Tropical</strong> lowland cloud <strong>for</strong>est” (LCF) has recently beendescribed in moist river valleys in French Guiana below 300 m. This <strong>for</strong>est resemblesmixed lowland rain <strong>for</strong>est, but the frequent occurrence of fog and thegreater richness of epiphytes sets this <strong>for</strong>est type apart.Integrating climatic and botanical research, a four year interdisciplinary projectinvestigating differences between LCF and tropical lowland rain<strong>for</strong>est (LRF) wasinitiated in 2007 supported by the German Research Foundation.Diversity of epiphytic bryophytes and pteridophytes, microclimate and epiphyticbiomass and cover on canopy trees in Central French Guiana were comparedbetween LCF and LRF. Analyses of these characteristics indicate that LCFresembles moist montane cloud <strong>for</strong>ests more than LRF, albeit at a far lower altitude.This similarity with montane cloud <strong>for</strong>ests can be explained by the increasedhumidity due to high fog frequencies observed in LCF, leading to greaterepiphytic biodiversity.TUESDAY 11:30 Hall H IVHere, we use statistical and geometrical methods <strong>for</strong> analysing the stem sizedistributions of tropical rain<strong>for</strong>ests, particularly maximum likelihood methods<strong>for</strong> statistical reconstruction of the stem size distribution and the concept ofsphere packing. We use field data from tropical <strong>for</strong>ests of different sites in Panamaand Malaysia (in total 61 ha).The applications of the abovementioned methods on these field data indicatethat the widely-spread assumption of a power-law <strong>for</strong> the stem size distributioncan not be substantiated.gtö<strong>Society</strong> <strong>for</strong> <strong>Tropical</strong> <strong>Ecology</strong> | Gesellschaft für Tropenökologie e.V. Status and future of tropical biodiversity | Frankfurt, 21 - 24 February 2011gtö