Taxonomy and Species Richness of Amazonian Pimplinae and Rhyssinae (hymenoptera: ichneumonidae)

The Amazonian region, the biggest rain forest of our planet, is known for its extraordinary biodiversity. Most of this diversity is still unexplored and new species of different taxa are regularly found there. In this region, as in most areas of the world, insects are some of the most abundant organisms. Therefore, studying this group is important to promote the conservation of these highly biodiverse ecosystems of the planet. Among insects, parasitoid wasps are especially interesting because they have potential for use as biodiversity indicators and biological control agents in agriculture and forestry. The parasitoid wasp family Ichneumonidae is one of the most species rich groups among the kingdom Animalia. This group is still poorly known in many areas of the world; the Amazonian region is a clear example of this situation. Ichneumonids have been thought to be species poor in Amazonia and other tropical areas. However, recent studies are suggesting that parasitoid wasps may be quite abundant in Amazonia and possibly in most tropical areas of the world. The aim of my doctoral thesis is to study the species richness and taxonomy of two of the best known ichneumonid subfamilies in the Neotropical region, Pimplinae and Rhyssinae. To do this I conducted two extensive sampling programs in the Peruvian Amazonia. I examined also a large number of Neotropical ichneumonids deposited to different natural history museums. According to the results of my thesis, the species richness of these parasitoids in the Amazonian region is considerably higher than previously reported. In my research, I firstly further develop the taxonomy of these parasitoids by describing many new species and reporting several new faunistic records (I, II, III). In this first part I focus on two genera (Xanthopimpla and Epirhyssa) which were thought to be rather species poor. My thesis demonstrates that these groups are actually rather species rich in the Amazonian region. Secondly, I concentrate on the species richness of these parasitoids in a global comparison showing that the Neotropical region and especially the Peruvian Amazonia is one of the most species rich areas of Pimpliformes ichneumonids (V). Furthermore, I demonstrate that with the data available to date no clear latitudinal gradient in species richness is visible. Thirdly, increasing the macroecological knowledge of these parasitoids I show that some previously unreported ichneumonid subfamilies are present in the Amazonian region (IV). These new insights and the results of the global comparison of ichneumonid inventories suggest that the previous belief of low diversity in the tropics is most likely related to a lack of sampling effort in the region. Overall, my research increases the knowledge of Neotropical ichneumonids highlighting the importance of Peruvian Amazonia as one of the diversity hotspots of parasitoid wasps.

El campesinado de la Amazonia colombiana : construcción territorial, colonización forzada y resistencias

Dans cette thèse nous démontrons que la paysannerie colombienne s'est constituée telle quelle, à partir de: 1) la construction et de la mise en œuvre des pratiques économiques et agro-productives compatibles avec l'environnement; 2) des habitus et des coutumes qu’elle a inventé et a récré à partir de l'interaction quotidienne avec sa famille et sa communauté et 3) de la lutte politique qu'elle a entrepris tant pour exiger à l'État sa reconnaissance sociale, territoriale et juridique, comme pour arrêter l'avance territoriale des entrepreneurs agraires. Par conséquent, la paysannerie ne peut pas être conçue comme une catégorie conceptuelle construite, a priori , définie dehors de l’histoire, comme un groupe social homogène, et avec caractéristiques égales à niveau global. La paysannerie colombienne, dans sa lutte politique pour la défense du territoire, a affronté à un entrepreneur agraire qui, orienté par une logique unidirectionnelle, élitiste et exclusive de « progrès » et du « développement », a nié à la paysannerie ses droits territoriaux, économiques, sociaux et culturels. De plus, en faisant un usage patrimonial de l’État, il l`a poursuivi, stigmatisé et expulsé de la communauté politique. La paysannerie a affronté un État et un entrepreneur agraire que, depuis l'État d’Exception et de la déclaration de la paysannerie comme “obstacle du développement” et “ennemi de la nation”, ils ont revendiqué le droit, inhérent des souverainetés classiques, de définir qui peut vivre et qui doit mourir. La dynamique historique et successive d'expropriation territoriale de la paysannerie et la mise en œuvre de ce qui est dénommé, dans cette thèse, nécro-politique agraire, ont été cachées dans le concept de “colonisation spontanée” et dans un discours qui présente au paysan comme « héros», «entrepreneur» et «constructeur de patrie», quand il a été obligé par raisons d'ordre économique, juridique et militaire, à entreprendre de nouveaux processus de colonisation forcée. La réponse de la paysannerie à cette dynamique a inclus des résistances de caractère intrasystémique et contre-systémique. Elle n'a jamais décliné à sa lutte par le droit à la terre – qui fait partie de son territoire et considère comme inaliénable - et à son droit d'avoir des droits. En étudiant le cas de la paysannerie de l'Amazonie colombienne, dans cette recherche, nous démontrons que la paysannerie a eu une grande capacité d'affronter les adversités économiques et politiques, et de s’inventer et de se refaire eux-mêmes dans nouveaux espaces. La paysannerie est un sujet social qui a refusé de façon entêtée et permanente, avec ses attitudes et ses actions, à obéir et à être domestiquée par les paramètres de la modernité. Elle s'est refusée à modifier ses dispositions internes et ses manières de voir le monde, son habitus et s’est reconstituée chaque jour dans une modernité qui menace sa subjectivité et son autonomie. La paysannerie formule des projets agro-écologiques, socioéconomiques et d'insertion politique dans un modèle du développement agraire qui insiste de le nier comme sujet avec des droits.

Monáitaga úai – Palabra que se hace amanecer : el cambio en las formas de “gobierno propio” entre la Gente de Centro del medio río Caquetá, Amazonia colombiana

Depuis la fin du XIXe siècle, des dynamiques sociales diverses – holocauste du caoutchouc, colonie pénale, missions catholiques, présence d’institutions gouvernementales et non gouvernementales — ont reconfiguré les formes d’organisation sociale des habitants du moyen fleuve Caquetá, dénommés Gens de centre. Nous nous arrêterons en particulier sur l’effet de ces changements sur leurs formes d’autonomie. Avec la reconnaissance par l’État, au cours des années 1980 et 1990, des peuples indigènes en tant que minorités ethniques, surgit une dichotomie entre ce qui est « traditionnel » autochtone, par opposition à ce qui est « moderne », étant donné les processus d’acculturation et inclusion de ces groupes dans la société majoritaire. Dans le présent travail, on établit une comparaison des figures « d’autorité traditionnelle » et de « leader », une différenciation faite dans la région du moyen fleuve Caquetá. Dans un premier temps, on donne un aperçu théorique de la figure de chef dans les terres basses de l’Amérique du Sud et sa validité et pertinence dans la situation du moyen fleuve Caquetá. Puis, l’on présente comment se forme l’autorité traditionnelle et ses champs d’action. On montre, de la même façon, les différents processus qui ont donné lieu à l’apparition de la figure de leader et les espaces où celle-ci évolue. La relation entre les deux figures est à la fois contradictoire et complémentaire. Finalement, on expose, avec des exemples concrets, les rapports entre les Gens de centre et les institutions gouvernementales et la remise en question de l’autonomie accordée aux groupes minoritaires dans la Constitution politique de la Colombie de 1991.

La Amazonia como elemento geopolítico determinante en la consolidación de Brasil como potencia regional (1988-2011)

La presente monografía busca analizar el papel geopolítico del Amazonas en el proceso de consolidación de Brasil como potencia regional, en el periodo de 1988 al 2011. Desde la democratización de Brasil en 1988, este país empezó a tener un papel destacado en la región debido a su liderazgo en los procesos de integración, estimulado por su intención de ser potencia regional. Ahora bien, esta pretensión no surge exclusivamente como efecto de los nuevos fenómenos de la posguerra fría, de hecho, tiene su origen con los postulados de la escuela geopolítica brasileña de mediados de 1930, donde nace la idea de un Brasil con un destino manifiesto de proyectarse continentalmente, que debe cumplir mediante el desarrollo del Amazonas. Por lo anterior, el Amazonas se consolida como un elemento determinante para Brasil como potencia regional, que por ende, ha definido el direccionamiento de sus políticas nacionales y regionales.

Response to comment on “The response of vegetation on the Andean flank in western Amazonia to Pleistocene climate change” – M.L. Cárdenas et al., Science 331, 1055 (25 February 2011)”.

Puyasena et al. question our interpretation of climate-driven vegetation change on the Andean flank in western Amazonia during the middle Pleistocene and suggest that the use of Podocarpus spp. as a proxy of past climate change should be reassessed. We defend our assertion that vegetation change at the Erazo study site was predominantly driven by climate change due to concomitant changes recorded by multiple taxa in the fossil record.

The response of vegetation on the Andean flank in western Amazonia to Pleistocene climate change

A reconstruction of past environmental change from Ecuador reveals the response of lower montane forest on the Andean flank in western Amazonia to glacial-interglacial global climate change. Radiometric dating of volcanic ash indicates that deposition occurred ~324,000 to 193,000 years ago during parts of Marine Isotope Stages 9, 7, and 6. Fossil pollen and wood preserved within organic sediments suggest that the composition of the forest altered radically in response to glacial-interglacial climate change. The presence of Podocarpus macrofossils ~1000 meters below the lower limit of their modern distribution indicates a relative cooling of at least 5°C during glacials and persistence of wet conditions. Interglacial deposits contain thermophilic palms suggesting warm and wet climates. Hence, global temperature change can radically alter vegetation communities and biodiversity in this region.

Environmental impact of geometric earthwork construction in pre-Columbian Amazonia

There is considerable controversy over whether pre-Columbian (pre-A.D. 1492) Amazonia was largely “pristine” and sparsely populated by slash-and-burn agriculturists, or instead a densely populated, domesticated landscape, heavily altered by extensive deforestation and anthropogenic burning. The discovery of hundreds of large geometric earthworks beneath intact rainforest across southern Amazonia challenges its status as a pristine landscape, and has been assumed to indicate extensive pre-Columbian deforestation by large populations. We tested these assumptions using coupled local- and regional-scale paleoecological records to reconstruct land use on an earthwork site in northeast Bolivia within the context of regional, climate-driven biome changes. This approach revealed evidence for an alternative scenario of Amazonian land use, which did not necessitate labor-intensive rainforest clearance for earthwork construction. Instead, we show that the inhabitants exploited a naturally open savanna landscape that they maintained around their settlement despite the climatically driven rainforest expansion that began ∼2,000 y ago across the region. Earthwork construction and agriculture on terra firme landscapes currently occupied by the seasonal rainforests of southern Amazonia may therefore not have necessitated large-scale deforestation using stone tools. This finding implies far less labor—and potentially lower population density—than previously supposed. Our findings demonstrate that current debates over the magnitude and nature of pre-Columbian Amazonian land use, and its impact on global biogeochemical cycling, are potentially flawed because they do not consider this land use in the context of climate-driven forest–savanna biome shifts through the mid-to-late Holocene.

Pre-Columbian ring ditch construction and land use on a “chocolate forest island” in the Bolivian Amazon

We present a palaeoecological investigation of pre-Columbian land use in the savannah “forest island” landscape of north-east Bolivian Amazonia. A 5700 year sediment core from La Luna Lake, located adjacent to the La Luna forest island site, was analysed for fossil pollen and charcoal. We aimed to determine the palaeoenvironmental context of pre-Columbian occupation on the site and assess the environmental impact of land use in the forest island region. Evidence for anthropogenic burning and Zea mays L. cultivation began ~2000 cal a BP, at a time when the island was covered by savannah, under drier-than-present climatic conditions. After ~1240 cal a BP burning declined and afforestation occurred. We show that construction of the ring ditch, which encircles the island, did not involve substantial deforestation. Previous estimates of pre-Columbian population size in this region, based upon labour required for forest clearance, should therefore be reconsidered. Despite the high density of economically useful plants, such as Theobroma cacao, in the modern forest, no direct pollen evidence for agroforestry was found. However, human occupation is shown to pre-date and span forest expansion on this site, suggesting that here, and in the wider forest island region, there is no truly pre-anthropogenic ‘pristine’ forest.

Concordant Phylogeographies of 2 Malaria Vectors Attest to Common Spatial and Demographic Histories

The phylogeography of South American lineages is a topic of heated debate. Although a single process is unlikely to describe entire ecosystems, related species, which incur similar habitat limitations, can inform the history for a subsection of assemblages. We compared the phylogeographic patterns of the cytochrome oxidase I marker from Anopheles triannulatus (N = 72) and previous results for A. darlingi (N = 126) in a broad portion of their South American distributions. Both species share similar population subdivisions, with aggregations northeast of the Amazon River, in southern coastal Brazil and 2 regions in central Brazil. The average (ST) between these groups was 0.39 for A. triannulatus. Populations northeast of the Amazon and in southeastern Brazil are generally reciprocally monophyletic to the remaining groups. Based on these initial analyses, we constructed the a priori hypothesis that the Amazon and regions of high declivity pose geographic barriers to dispersal in these taxa. Mantel tests confirmed that these areas block gene flow for more than 1000 km for both species. The efficacy of these impediments was tested using landscape genetics, which could not reject our a priori hypothesis but did reject simpler scenarios. Results form summary statistics and phylogenetics suggest that both lineages originated in central Amazonia (south of the Amazon River) during the late Pleistocene (579 000 years ago) and that they followed the same paths of expansion into their contemporary distributions. These results may have implications for other species sharing similar ecological limitations but probably are not applicable as a general paradigm of Neotropical biogeography.

Spatial expansion and population structure of the neotropical malaria vector, Anopheles darlingi (Diptera: Culicidae)

Extensive population structuring is known to occur in Anopheles darlingi, the primary malaria vector of the Neotropics. We analysed the phylogeographic structure of the species using the mitochondrial cytochrome oxidase I marker. Diversity is divided into six main population groups in South America: Colombia, central Amazonia, southern Brazil, south-eastern Brazil, and two groups in north-east Brazil. The ancestral distribution of the taxon is hypothesized to be central Amazonia, and there is evidence of expansion from this region during the late Pleistocene. The expansion was not a homogeneous front, however, with at least four subgroups being formed due to geographic barriers. As the species spread, populations became isolated from each other by the Amazon River and the coastal mountain ranges of south-eastern Brazil and the Andes. Analyses incorporating distances around these barriers suggest that the entire South American range of An. darlingi is at mutation-dispersal-drift equilibrium. Because the species is distributed throughout such a broad area, the limited dispersal across some landscape types promotes differentiation between otherwise proximate populations. Moreover, samples from the An. darlingi holotype location in Rio de Janeiro State are substantially derived from all other populations, implying that there may be additional genetic differences of epidemiological relevance. The results obtained contribute to our understanding of gene flow in this species and allow the formulation of human mosquito health protocols in light of the potential population differences in vector capacity or tolerance to control strategies. (C) 2009 The Linnean Society of London, Biological Journal of the Linnean Society, 2009, 97, 854-866.

Caries, gender and socio-economic change in the Xavante Indians from Central Brazil

Background: The oral health conditions of indigenous peoples in Amazonia are closely associated with ecological and dietary changes related to interaction with non-Indians. Aim: The study investigated the incidence of caries in an indigenous community from Central Brazil focusing on gender differences. Subjects and methods: The research was conducted among the Xavante Indians and was based on longitudinal data collected in two surveys (1999 and 2004). The study included 128 individuals, 63 (49.2%) males and 65 (50.8%) females, divided in four age brackets (6-12, 13-19, 20-34, 35-60 years of age). The DMFT (decayed, missing and filled teeth) index and incidences (difference between 1999 and 2004) were calculated for each individual. The proportion of incidence was also calculated. Differences in caries risk between gender and age brackets were compared by parametric and non-parametric tests. Results: There were statistically significant differences in relation to caries incidence between age brackets and gender. The greatest incidence was observed in the 20-34 age bracket, which presented 3.30 new decayed teeth, twice the risk of the 6-12 age bracket (p0.01), chosen as reference. While females in most age groups did not show higher risk for caries when compared to males, there was a 4.04-fold risk in the 20-34 age bracket (p0.01). Conclusion: It is concluded that factors related to the social functions of each sex (gender issues) and differential access to information, health services, and education may help to understand the differences observed in the incidence of caries.

Atmospheric versus vegetation controls of Amazonian tropical rain forest evapotranspiration: Are the wet and seasonally dry rain forests any different?

This study analyzes evapotranspiration data for three wet and two seasonally dry rain forest sites in Amazonia. The main environmental (net radiation, vapor pressure deficit, and aerodynamic conductance) and vegetation (surface conductance) controls of evapotranspiration are also assessed. Our research supports earlier studies that demonstrate that evapotranspiration in the dry season is higher than that in the wet season and that surface net radiation is the main controller of evapotranspiration in wet equatorial sites. However, our analyses also indicate that there are different factors controlling the seasonality of evapotranspiration in wet equatorial rain forest sites and southern seasonally dry rain forests. While the seasonality of evapotranspiration in wet equatorial forests is driven solely by environmental factors, in seasonally dry forests, it is also biotically controlled with the surface conductance varying between seasons by a factor of approximately 2. The identification of these different drivers of evapotranspiration is a major step forward in our understanding of the water dynamics of tropical forests and has significant implications for the future development of vegetation-atmosphere models and land use and conservation planning in the region.

Cloud streets and land-water interactions in the Amazon

Cloud streets are common feature in the Amazon Basin. They form from the combination of the vertical trade wind stress and moist convection. Here, satellite imagery, data collected during the COBRA-PARA (Caxiuan Observations in the Biosphere, River and Atmosphere of Para) field campaign, and high resolution modeling are used to understand the streets` formation and behavior. The observations show that the streets have an aspect ratio of about 3.5 and they reach their maximum activity around 15:00 UTC when the wind shear is weaker, and the convective boundary layer reaches its maximum height. The simulations reveal that the cloud streets onset is caused by the local circulations and convection produced at the interfaces between forest and rivers of the Amazon. The satellite data and modeling show that the large rivers anchor the cloud streets producing a quasi-stationary horizontal pattern. The streets are associated with horizontal roll vortices parallel to the mean flow that organizes the turbulence causing advection of latent heat flux towards the upward branches. The streets have multiple warm plumes that promote a connection between the rolls. These spatial patterns allow fundamental insights on the interpretation of the Amazon exchanges between surface and atmosphere with important consequences for the climate change understanding.