Integrated palaeoecology and archaeology: a powerful approach for understanding pre-Columbian Amazonia

The old paradigm that Amazonia's tropical ecosystems prevented cultural development beyond small-scale shifting agricultural economies, that had little environmental impact, no longer holds true for much of Amazonia. A diversity of archaeological evidence, including terra preta soils, raised fields, causeways, large habitation mounds, geometric earthworks, and megalithic monuments, all point to considerable cultural complexity and environmental impacts. However, uncertainty remains over the chronology of these cultures, their diet and economy, and the scale of environmental impact and land use associated with them. Here, we argue that a cross-disciplinary approach, closely coupling palaeoecology and archaeology, can potentially resolve these uncertainties. We show how, with careful site selection (pairing small and large lakes, close proximity to archaeological sites, transects of soil pits) and choice of techniques (e.g., pollen, phytoliths, starch grains, charcoal, stable isotopes), these two disciplines can be successfully integrated to provide a powerful tool for investigating the relationship between pre-Columbian cultures and their environment.

Pre-Columbian landscape impact and agriculture in the Monumental Mound region of the Llanos de Moxos, lowland Bolivia

We present a multiproxy study of land use by a pre-Columbian earth mounds culture in the Bolivian Amazon. The Monumental Mounds Region (MMR) is an archaeological sub-region characterized by hundreds of pre-Columbian habitation mounds associated with a complex network of canals and causeways, and situated in the forest–savanna mosaic of the Llanos de Moxos. Pollen, phytolith, and charcoal analyses were performed on a sediment core from a large lake (14 km2), Laguna San José (14°56.97′S, 64°29.70′W).We found evidence of high levels of anthropogenic burning from AD 400 to AD 1280, corroborating dated occupation layers in two nearby excavated habitation mounds. The charcoal decline pre-dates the arrival of Europeans by at least 100 yr, and challenges the notion that the mounds culture declined because of European colonization. We show that the surrounding savanna soils were sufficiently fertile to support crops, and the presence of maize throughout the record shows that the area was continuously cultivated despite land-use change at the end of the earthmounds culture. We suggest that burning was largely confined to the savannas, rather than forests, and that pre-Columbian deforestation was localized to the vicinity of individual habitation mounds, whereas the inter-mound areas remained largely forested.

Evaluating microfossil content of dental calculus from Brazilian sambaquis

To date, limited numbers of dental calculus samples have been analyzed by researchers in diverse parts of the world. The combined analyses of these have provided some general guidelines for the analysis of calculus that is non-destructive to archaeological teeth. There is still a need for a quantitative study of large numbers of calculus samples to establish protocols, assess the level of contamination, evaluate the quantity of microfossils in dental calculus, and to compare analysis results with the literature concerning the biology of calculus formation. We analyzed dental calculus from 53 teeth from four Brazilian sambaquis. Sambaquis are the shell-mounds that were established prehistorically along the Brazilian coast. The analysis of sambaqui dental calculi shows that there are relatively high concentrations of microfossils (phytoliths and starch), mineral fragments, and charcoal in dental calculus. Mineral fragments and charcoal are possibly contaminants. The largest dental calculi have the lowest concentrations of microfossils. Biologically, this is explained by individual variation in calculus formation between people. Importantly, starch is ubiquitous in dental calculus. The starch and phytoliths show that certainly Dioscorea (yam) and Araucaria angustifolia (Parana pine) were eaten by sambaqui people. Araceae (arum family), Ipomoea batatas (sweet potato) and Zea mays (maize) were probably in their diet. (C) 2009 Elsevier Ltd. All rights reserved.

Development of mound-building in Australian brush-turkeys (Alectura lathami) : the role of learning, testosterone and body mass

Australian brush-turkeys (Alectura lathami) hatch in incubation mounds of organic material and have no parental role models to learn from. When raised in outdoor aviaries, without adults, four of six males built incubation mounds at an early age of 4.5–9 months. The two males without mounds were the only ones without detectable levels of testosterone (T) at 4.5 months, whereas body mass did not explain the presence or absence of mound building. At the age of 11 months, all males had detectable T, including those without mounds. This study also investigated the development of social dominance in males kept in mixed-sex groups for 4.5 months. At this latter age, higher-ranked males tended to have higher T levels (P = 0.076), whereas dominance ranks at 4.5 months were not correlated with body mass or size, either at this age or at hatching. Overall, these results suggest that mound building develops without learning, and there is a relationship between T levels and dominance status as well as the absence or presence of mound building. These findings contribute to discussions on the role of learning in behavioural development and the role of T and body mass in avian life history.

Sedimentação carbonática de algas vermelhas coralináceas da plataforma continental da bacia de campos um modelo carbonático análogo para o terciário

O presente trabalho faz uma análise da plataforma continental média e externa da porção central da Bacia de Campos, entre as batimetrias de 65 e 300 metros. Nesta porção da plataforma são encontrados depósitos sedimentares formados por carbonatos e, secundariamente, por siliciclásticos com influência carbonática. Os carbonatos do Membro Grussaí da Formação Emborê se configuram como os mais importantes sedimentos presentes na área de estudo, sendo compostos majoritariamente por algas vermelhas coralináceas (lithothamniun). Os depósitos algálicos ocorrem sob duas formas: a) formas livres formando concreções nodulares centimétricas (rodolitos) e grainstones. b) Incrustações, formando substratos crustosos e lineamentos. Para a análise destes depósitos foram utilizados dados sísmicos tridimensionais relativos à seção terciária da Bacia de Campos e principalmente do fundo marinho. A associação destes dados com amostras de fundo e filmagens do fundo marinho ao longo do traçado de dutos de escoamento de hidrocarbonetos, permitiu a definição de um modelo de distribuição faciológica para os carbonatos formados por algas vermelhas coralináceas e feições fisiográficas associadas a eles. A morfologia do fundo do mar foi dividida em províncias fisiográficas diretamente relacionadas com o padrão deposicional das algas vermelhas e, secundariamente, por sedimentos siliciclásticos. Os padrões morfológicos refletem a presença de bancos carbonáticos de morfologia rugosa, lineamentos carbonáticos em forma de cristas com direção paralela à linha de costa atual, lineamentos em forma de barras obliquas à linha de costa atual, e platôs ou patamares, caracterizados por relevo suave Os sedimentos de fundo foram agrupados em seis fácies sedimentares, as quais estão relacionadas com a morfologia do fundo marinho: (a) Fácies Areias Siliciclásticas com Bioclastos - depositada nos patamares e formada por sedimentos mistos. (b) Fácies Grainstones com Rodolitos – desenvolve-se nos patamares e é composta, basicamente, por grainstones dominados por algas vermelhas, rodolitos e, secundariamente, por areias siliciclásticas. (c) Fácies Boundstone Ridges – relaciona-se com a formação dos lineamentos carbonáticos paralelos à linha de costa; apresentam grainstones e rodolitos na base dos lineamentos e um predomínio de boundstones nas partes altas; marcam a passagem entre patamares. (d) Fácies Boundstone Mounds - relaciona-se fisiograficamente aos lineamentos de barras carbonáticas com orientação obliqua à linha de costa, e se localizam no interior dos patamares. (e) Fácies Boundstone Banks e Grainstones - corresponde a bancos carbonáticos de relevo irregular e que resultam da bioconstrução algálica sob forma de boundstones, com deposição de grainstones nos interbancos. (f) Fácies Mista - posicionada no talude superior, é resultado da mescla entre os sedimentos siliciclásticos de granulometria silte até areia muito fina com lamas e areias carbonáticas. A distribuição faciológica das algas vermelhas coralináceas presentes na área de estudo se desenvolve em batimetrias muito superiores ao que normalmente é esperado para os carbonatos. Sua atividade se desenvolve desde a batimetria de 45 m até 150 m, sendo que o intervalo mais produtivo ocorre entre 55 e 90 m Esses valores decorrem da análise de incrustações presentes em dutos situados na plataforma e talude continental. Outra indicação da existência de deposição em batimetrias mais elevadas é a presença de relictos de boundstones entre as atuais batimetrias de 170 a 230 m. Estes relictos indicam que, durante o rebaixamento do nível do mar de 120 m que ocorreu no final do Pleistoceno, a fábrica carbonática responsável por estes depósitos permaneceu ativa em batimetrias próximas a 50 e 110 m. Por estarem se desenvolvendo em batimetrias elevadas, os depósitos sedimentares estão submetidos aos efeitos hidrodinâmicos de correntes marinhas, principalmente a Corrente do Brasil. Devido a isto, a distribuição faciológica dos carbonatos algálicos apresenta diferença quando comparada com o ambiente convencional de deposição carbonática. Os substratos dos principais lineamentos carbonáticos, posicionados nas atuais cotas batimétricas de 110 m, 100 m, 85 m e 70 m, são interpretados como decorrentes das estabilizações episódicas de linha de praia que ocorreram durante o último processo transgressivo. A erosão desenvolvida pelas ondas nestas paleolinhas de praia esculpiu pequenas escarpas que serviram de substrato para a instalação posterior da Fácies Boundstone Ridges a partir de batimetrias entre 45 a 50 m. O substrato gerado nos patamares não desenvolveu rigidez suficiente para a instalação de formas incrustantes, exceto onde a remobilização do fundo marinho, durante o último evento transgressivo, desenvolveu formas de leitos tipo dunas transversas que serviram de substrato para a deposição da Fácies Boundstone Mounds, as quais atualmente estão estabilizadas pelas incrustrações de boundstones O modelo de deposição de algas coralináceas de “águas profundas” proposto neste trabalho pode ser o mais apropriado como análogo para a sedimentação dominada por algas vermelhas do Terciário das bacias meridionais Brasileiras, quando não houver uma clara associação com outros constituintes carbonáticos exclusivos de águas rasas. Uma evidência que sinaliza a viabilidade deste modelo decorre da interpretação e análise de atributos sísmicos da seção Terciária da Bacia de Campos, onde as feições carbonáticas, semelhantes às encontradas no recente, tendem a se repetir com freqüência.

Growth evolution of ZnO thin films deposited by RF magnetron sputtering

We study the surface morphology evolution of ZnO thin films grown on glass substrates as a function of thickness by RF magnetron sputtering technique. The surface topography of the samples is measured by atomic force microscopy (AFM). All AFM images of the films are analyzed using scaling concepts. The results show that the surface morphology is initially formed by a small grains structure. The grains increase in size and height with growth time resulting in the formation of a mounds-like structure. The growth exponent, beta, and the exponent defining the evolution of the characteristic wavelength of the surface, p, amounted to beta = 0.76 +/- 0.08 and p = 0.3 +/- 0.05. From these exponents, the surface morphology is determined by the nonlocal shadowing effects, that is the dominant mechanism, due to the incident deposition particles during film growth.

Nest architecture of the leaf-cutting ant Acromyrmex rugosus rugosus

The prominent nests mounds of many ant species are one of the most obvious signs of their presence, yet the subterranean architecture of nests is often poorly known. The present work aimed to establish the external and internal structure of nests of a species of leaf-cutting ant, Acromyrmex rugosus rugosus, by either marking the interior of nests with talcum powder, or forming casts with cement. Twelve nests were excavated and surveyed, with eight being marked with talcum powder and four cast with cement. The external and internal structure of the nests was highly variable. The largest and smallest nests had mound areas of 9.89 m(2) and 0.01 m(2) respectively. The number of chambers found ranged from I to 26, with maximum dimensions of between 6 and 70 cm. Chambers were found close to the soil surface (6 cm) down to a maximum depth of 3.75 m. In addition to chambers containing fungus garden, some chambers were found to be empty, filled with soil or filled with waste, the first time this has been recorded in a species of Acromyrmex. The nests of A. rugosus rugosus appear to be unusually complex for the genus, containing a diversity of irregular chambers and tunnels.

FIRE ANT MOUND DENSITIES IN THE UNITED-STATES AND BRAZIL (HYMENOPTERA, FORMICIDAE)

To compare fire ant populations (Solenopsis) in North and South America, we surveyed 102 preselected roadside sites, half in the southeastern United States and half in the state of Mato Grosso do Sul, Brazil. Fire ants were considerably more abundant in the United States. They occurred at more sites (100 versus 70%), in higher densities (170 versus 30 mounds/ha), in larger mounds (27.0 versus 13.8 liters), and they constituted a larger fraction of the local ant community (97 versus 13% of occupied baits). These data are consistent with the hypothesis that North American populations of S. invicta have escaped natural biological control; however, cultural and climatic factors are also likely explanations.

Occurrence of polygyny in Procornitermes araujoi (Termitidae, Nasutitermitinae)

Procornitermes araujoi is a mandibulate termite of the Nasutitermitinae subfamily that builds mounds in savannas of the Central and Southeastern regions of Brazil. This paper reports the occurrence of three imaginai queens in the same nest of this termite located in Rio Claro, (SP), Brazil. The associated queens were similar in size, degree of physogastry, and pigmentation. The king was not found. The polygyny and nest architecture of P. araujoi are discussed.

Avaliação de quatro métodos de restauração florestal de áreas úmidas degradadas no Município de Mineiros do Tietê - SP

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Radarfacies and sedimentological analysis: study of sedimentary substrate from an archaeological site (shell mound), southern Brazil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

BADGERS (Taxidea taxus) AS OCCASIONAL PESTS IN AGRICULTURE

The badger (Taxidea taxus). because of its strong propensity for digging, is considered North America's fossorial carnivore, feeding mostly on ground squirrels, pocket gophers, and mice throughout much of the western and midwestern continent. Badger excavations, primarily in search of food, produce mounds and deep holes which can damage alfalfa and other crops and damage farm equipment and water systems. Depredations include poultry, waterfowl, and eggs. Overall, the badger is considered a relatively minor vertebrate pest. As a furbearer it is considered a renewable natural resource. Most local pest problems are currently reduced through leghold trapping and shooting. Habitat modification through continuous rodent control is effective and a long-lasting badger control method.

Archaeofacies Analysis: Using Depositional Attributes to Identify Anthropic Processes of Deposition in a Monumental Shell Mound of Santa Catarina State, Southern Brazil

In the coast of Santa Catarina State (southern Brazil), a large population of monumental shell mounds characterizes a highly dynamic coastal setting. In this paper, sedimentary facies analysis was adapted for description, sampling, and interpretation of shell mound complex and repetitive archaeostratigraphic successions. Archaeofacies identification in the field, according to depositional attributes, is tested by contrasting field description with multi-element chemical analyses, total carbon and nitrogen determinations, and micromorphological descriptions. Two vertical sequences at the black deposit of Jabuticabeira II shell mound were studied and preliminary results showed that: (1) depositional attributes are a reliable base for archaeofacies identification in the field, (2) the formation process of this site involved a sequence of anthropic depositional processes, where burned refuse was redeposited over the shell mound following a ritual construction pattern, and (3) the black deposit includes a double palimpsest that refers to provenance and meaning of mound construction material. (C) 2009 Wiley Periodicals, Inc.

Multifemale nests and social behavior in Euglossa melanotricha (Hymenoptera,Apidae, Euglossini)

The nesting biology and social behavior of the euglossine bee species Euglossa melanotricha was analyzed based on the monitoring of eight nests found in man-made cavities and transferred to observation boxes. Euglossa melanotricha females usually construct their nests in cavities in the ground, in buildings, or in mounds. In this study, we present new data on the nesting biology of E. melanotricha. The process of reactivation of nests was commonly observed with one to three females participating in the reactivation. The duration of the process of reactivation ranged from 10 to 78 days (n = 31) and were longer during the rainy season. Time spent (in days) for provisioning, oviposition and closing a single cell was higher in reactivations that occurred during the dry period. 151 emergences were observed (39 males and 112 females). 90 (80.3%) of the emerged females returned to the natal nest, but only 35(38.9%) remained and actively participated in the construction and provisioning of cells. The other 55 abandoned the nests after several days without performing any work in the nest. Matrifilial nest structure was regulated by dominance-subordinate aggressive behavior among females, where the dominant female laid almost all eggs. Task allocation was recognized by behavioral characteristics, namely, agonism and oophagy in cells oviposited by other females. Euglossa melanotricha is multivoltine and its nesting is asynchronous with respect to season. Our observations suggest a primitively eusocial organization. These observations of E. melanotricha provide valuable information for comparison with other species of Euglossa in an evolutionary context.

Human-environment interactions in pre-Columbian Amazonia: The case of the Llanos de Moxos, Bolivia

The reconstruction of past environmental and historical events is much needed in Amazonia, a region at the centre of heated debates about the extent of pre-Columbian human disturbance of the natural ecosystems. Important aspects of this debate are to establish to what extent the rise of social complexity was influenced by the local geo-ecology; and what productive strategies were adopted in order to sustain these societies. The Llanos de Moxos (LM), in the Bolivian Amazon, is a vast floodplain made up of a variety of geo-ecological sub regions that host many different types of pre-Columbian earthworks. Therefore, it offers an excellent opportunity to compare different kinds of archaeological landscapes and their relationship to different pre-Columbian cultures and environmental settings. This paper analyses the links between pre-Columbian earthworks and the local geo-ecology in two regions of the LM: 1) the platform field region (PFR) in the north of Santa Ana de Yacuma, where the highest concentration of raised fields has been documented, and 2) the monumental mounds region (MMR) south and east of Trinidad, where >100 pre-Columbian monumental mounds are found. The study draws from remote sensing and GIS analysis, field work in the Bolivian lowlands, and laboratory analysis. Differences in the way people transformed the landscape in the PFR and MMR seem to respond to differences in the local geo-ecology of the two sites. The results also suggest that environmental conditions exerted an important, though not exclusive, control over the levels of social complexity that were reached in different areas of the LM.