A molecular phylogenetic analysis of diversification in Amazonian Anolis lizards

We present a mitochondrial DNA (mtDNA) haplotype phylogeny for Amazonian Anolis lizards, including geographical sampling within four species distributed across the Amazon basin (A. fuscoauratus, A. nitens, A. ortonii and A. punctatus). Approximately 1500 bp of mtDNA encoding ND2, COI and four transfer RNAs (tRNAs) are reported for 39 specimens representing four to five populations of each widespread species, plus eight outgroups. These new sequences are aligned with eight previously published sequences, yielding 914 variable characters and 780 parsimony-informative characters. Phylogenetic analyses using maximum parsimony and maximum likelihood reject the hypothesis that Amazonian anoles form a monophyletic group excluding Central American and Caribbean anoles, and suggest multiple faunal exchanges among these regions. Haplotype divergence among geographical populations of A. nitens, whose variation was influential in formulating the Pleistocene refuge hypothesis of Amazonian speciation, is very large (13-22% sequence difference), suggesting that these populations separated well before the Pleistocene. Haplotype divergences among geographical populations of A. fuscoauratus (3-4%), A. punctatus (4-9%) and A. ortonii (6-8%) also indicate pre-Pleistocene differentiation within each species, but temporally incongruent patterns among species.     

Competing paradigms of Amazonian diversification and the Pleistocene refugium hypothesis

Evidence from butterflies and birds suggests that most extant Amazonian species arose during the Pleistocene (< 2.6 Ma). If these speciation events share common, extrinsic causes, their explanation probably involves climate‐driven biogeographical shifts, because the major orogenic events shaping the biogeography of the Neotropics were over by then. In the light of these observations, criticisms of the Pleistocene refugium hypothesis are examined.     

The regional variation of aboveground live biomass in old-growth Amazonian forests

The biomass of tropical forests plays an important role in the global carbon cycle, both as a dynamic reservoir of carbon, and as a source of carbon dioxide to the atmosphere in areas undergoing deforestation. However, the absolute magnitude and environmental determinants of tropical forest biomass are still poorly understood. Here, we present a new synthesis and interpolation of the basal area and aboveground live biomass of old‐growth lowland tropical forests across South America, based on data from 227 forest plots, many previously unpublished. Forest biomass was analyzed in terms of two uncorrelated factors: basal area and mean wood density. Basal area is strongly affected by local landscape factors, but is relatively invariant at regional scale in moist tropical forests, and declines significantly at the dry periphery of the forest zone. Mean wood density is inversely correlated with forest dynamics, being lower in the dynamic forests of western Amazonia and high in the slow‐growing forests of eastern Amazonia. The combination of these two factors results in biomass being highest in the moderately seasonal, slow growing forests of central Amazonia and the Guyanas (up to 350 Mg dry weight ha^?1) and declining to 200–250 Mg dry weight ha^?1 at the western, southern and eastern margins. Overall, we estimate the total aboveground live biomass of intact Amazonian rainforests (area 5.76 × 10⁶ km² in 2000) to be 93±23 Pg C, taking into account lianas and small trees. Including dead biomass and belowground biomass would increase this value by approximately 10% and 21%, respectively, but the spatial variation of these additional terms still needs to be quantified.     

不同恢复阶段热带森林土壤nirS型反硝化微生物群落结构及多样性特征

探明热带森林土壤反硝化微生物群落结构及多样性,对于理解反硝化引起的N₂O排放及缓解全球变暖具有重要意义。本研究以西双版纳3个不同恢复阶段热带森林类型[即白背桐（Mallotus paniculatus,MP）、崖豆藤（Millttia leptobotrya,ML）群落、群落及高檐蒲桃（Syzygium oblatum,SO）群落]为研究对象,揭示土壤nirS型反硝化微生物群落组成及多样性的干湿季变化,分析热带森林恢复过程中土壤理化环境变化对nirS型反硝化细菌群落的影响。结果表明,变形菌门（Proteobacteria）和酸杆菌门（Acidobacteria）相对丰度表现为恢复前期高于恢复后期,而脱氯单胞菌属（Dechloromonas）、嗜盐单胞菌属（Halomonas）和罗思河小杆菌属（Rhodanobacter）表现为恢复后期高于恢复前期;绿弯菌门（Chloroflexi）和放线菌门（Actinobacteria）均随恢复年限增加而增加,而贪铜菌属（Cupriavidus）和假单胞菌属（Pseudomonas）的相对丰度表现为随恢复年限增加而降低。9月份各样地新检测出的属数量表现为：SO （19种） > MP （13种） > ML （7种）。土壤nirS型反硝化微生物群落的Shannon多样性指数表现为：高檐蒲桃群落 > 崖豆藤群落 > 白背桐群落,且9月（湿季） > 3月（干季）。相关分析表明,热带森林恢复引起土壤N库（全氮、NH₄⁺、NO₃^-）、C有效性（微生物量碳、易氧化碳）及微气候（土壤含水率与温度）的改变,能够显著影响nirS型反硝化细菌群落的结构及多样性。主成分分析结果表明,土壤硝态氮、微生物量碳、全氮及易氧化碳是调控不同恢复阶段热带森林土壤nirS型反硝化细菌群落结构及多样性变化的主控因子,其次为土壤水分、温度、水解氮、pH、铵态氮、有机碳、容重及C/N。     

Biotic resistance to invasion is ubiquitous across ecosystems of the United States

The biotic resistance hypothesis predicts that diverse native communities are more resistant to invasion. However, past studies vary in their support for this hypothesis due to an apparent contradiction between experimental studies, which support biotic resistance, and observational studies, which find that native and non‐native species richness are positively related at broad scales (small‐scale studies are more variable). Here, we present a novel analysis of the biotic resistance hypothesis using 24 456 observations of plant richness spanning four community types and seven ecoregions of the United States. Non‐native plant occurrence was negatively related to native plant richness across all community types and ecoregions, although the strength of biotic resistance varied across different ecological, anthropogenic and climatic contexts. Our results strongly support the biotic resistance hypothesis, thus reconciling differences between experimental and observational studies and providing evidence for the shared benefits between invasive species management and native biodiversity conservation.     

The implications of Tertiary and Quaternary sea level rise events for avian distribution patterns in the lowlands of northern South America

Aim To assess the correspondence between current avian distributions in the lowlands of northern South America with respect to the hypothesized importance of sea level rise and other events over the past 15 million years on speciation. Location Tropical lowlands of north‐western South America. Methods To establish which bird taxa may have originated in each area of endemism, I examined the ranges of all bird species occurring in the Pacific and the Caribbean lowlands. To determine land and sea distribution during a sea level rise of 100 m in north‐western South America and eastern Central America, I traced the 100 m contour line from the Geoatlas of Georama and the Global 30‐Arc‐Second Elevation Data (GTOPO30) produced by the US Geological Survey. Results During a sea level rise of ～100 m, marine incursions would have occurred from the Caribbean Sea and the Pacific Ocean. Several areas of tropical forest and dry/arid vegetation would have been isolated, currently known as the Darién, Chocó, Nechí, Catatumbo, Tumbesian and Guajiran areas of animal and plant endemism. Main conclusions A large part of the high diversity of forest and nonforest birds and other animals and plants in the Pacific rain forest and the Caribbean woodland likely arose as the result of sea level rises, dispersal and other geological and climatic events.