The area postrema: a cardiovascular control centre at the blood-brain interface?

The area postrema (AP) is one of the circumventricular organs of the brain and as such it is highly vascular and lacks the normal blood-brain barrier. Anatomical tracing studies have demonstrated afferent projections to AP originating from the paraventricular nucleus, lateral parabrachial nucleus (l-PBN), nucleus tractus solitarius (NTS), as well as the vagus nerve. AP neurons have been shown to project primarily to l-PBN, and NTS. Receptor localization studies have reported dense aggregations of many specific peptide receptors in AP including those for angiotensin II (ANG), atrial natriuretic peptide (ANP), and endothelin (ET). Electrical stimulation studies have shown that activation of AP neurons at low frequencies (less than 15 Hz) results in decreases in blood pressure and heart rate, while higher frequency (greater than 20 Hz) stimulation causes increases in blood pressure. These low frequency effects on blood pressure and heart rate appear to result from activation of separate components of the autonomic nervous system. Extracellular single unit recordings have identified two functionally separate populations of AP neurons: one responsive to circulating ANG and a second apparently responsive to changes in blood pressure. In addition, AP neurons are activated by increases in circulating ET. Afferent inputs to AP neurons from 1-PBN have separate excitatory (12% of AP neurons) or inhibitory (12% of AP neurons) effects on a relatively small proportion of AP neurons. In contrast, preliminary evidence suggests a much more broadly distributed excitatory input to approximately 70% of tested AP neurons originating from the aortic depressor nerve. These studies provide considerable evidence implicating the AP as a significant neural structure regulating the cardiovascular system.     

The Upper Paleolithic triple burial of Dolní Vestonice: pathology and funerary behavior

This work focuses on paleopathological analysis of one of the skeletons from the Gravettian triple burial of Dolní Vestonice (Moravia) and addresses issues of Upper Paleolithic funerary behavior. The burial includes the well-preserved skeletons of three young individuals. The skeleton in the middle (DV 15) is pathological and very problematic to sex; the other two (DV 13 and DV 14) are males and lie in an unusual position. The young age, the possibility of a simultaneous interment, and the position of the three specimens have given rise to speculations about the symbolic significance of this spectacular and intriguing funerary pattern. The pathological condition of the skeleton in the middle further emphasizes its peculiarity. Main pathological changes of the DV 15 skeleton include: asymmetric shortening of the right femur and of left forearm bones, bowing of the right femur, right humerus, and left radius, elongation of fibulae, dysplasias of the vertebral column, and very marked enamel hypoplasias. Scrutiny of the medical literature suggests that the most likely etiology is chondrodysplasia calcificans punctata (CCP) complicated by trauma and early fractures of the upper limbs. CCP is a rare inherited disorder characterized by stippled ossification of the epiphyses. The cartilaginous stippling is a transient phenomenon that disappears during infancy, leaving permanent deformities on affected bones. Among the different forms of CCP, the X-linked dominant form is that resulting in asymmetric shortening and is lethal during early infancy in males. Thus, survival of DV 15 until young adult age would require the specimen to be a female. Clinical findings often associated with the disease (erythemas, ichthyosis, alopecia, cataracts, and joint contractures, among others) would emphasize the singular aspect of this individual, pointing to a condition that should be carefully taken into account when speculating on the significance of that peculiar burial.     

Seasonal variations of the middle-upper paleolithic transition at El castillo, Cueva Morín and El pendo (Cantabria, Spain)

With debate escalating in regard to the prolonged contemporaneity of neandertal and modern human groups in the Franco-Cantabrian region on the one hand, and the late persistence of neandertals (until ca. 28-30,000 B.P.) and Mousterian industries in southern Iberia on the other; sites with Mousterian-Upper Paleolithic sequences from northern Spain play a pivotal role in the ongoing investigation of the Middle-Upper Paleolithic transition in western Europe. An important line of inquiry into the nature of social and economic change from the Middle to Upper Paleolithic is the monitoring of shifts in land use and resource procurement patterns. The recognition of short-term, seasonal patterning in settlement and resource provisioning may provide insights into changes in mobility, territoriality, and social organization that might otherwise be missed. This paper presents results of a seasonality study of fauna from archaeological levels spanning the Middle-Upper Paleolithic transition from the sites of El Castillo, El Pendo, and Cueva Morín in Cantabrian Spain. Data concerning season of death and age at death of prey animals presented here are derived from dental growth mark (increment, annuli) analysis. These data, along with other artifactual and faunal evidence suggest to us that: (1) economic strategies and technologies pervasive in the Upper Paleolithic are rooted in the Cantabrian Middle Paleolithic; and, (2) the apparent increase in deposits from the Middle through Upper Paleolithic may be the signature of a gradual increase in logistical economic strategies including the heightened level of social organization required for their implementation.     

Plant tempering of Predynastic pisé at Adaïma in Upper Egypt: building material and taphonomy

Macroscopic plant remains found in pisé material (clay or mud used in building), used as lining in pits at the Upper Egyptian Predynastic site of Adaïma were investigated. Comparison with assemblages from the sediment fills of these pits and with assemblages from other contexts in the same site demonstrated the taphonomical importance of pisé as a building material for the formation of the sites archaeological sediment. In particular, the influence of the pisé plant temper on the composition of plant assemblages in the sediment fills of the pits was brought to the fore. The choice of specific plant materials for their use as temper in pisé or mud bricks is shown, in particular that of barley (Hordeum vulgare) threshing remains. The importance of cereal processing by-products as construction material is also assessed in a wider economic context and compared with later Egyptian mud brick plant contents.     

The depositional context of the early upper paleolithic human fossils from the Koneprusy (Zlatý kůn) and Mladec caves, Czech republic

The caves of Mladec I and II (Moravia) and Koneprusy (Bohemia) are principal hominid Early Upper Paleolithic sites in Central Europe that require a complex reconsideration from several viewpoints. The focus of this paper is on the depositional context of human fossils, which is clearer from the documentation of Koneprusy, excavated during the 1950s, than from the early reports about Mladec. Both caves are multi-floor underground karstic systems penetrated by vertical fissures and chimneys, where the fossils were found in restricted areas, related to debris cones accumulated under the chimneys. These associations are confirmed using Surfer reconstruction of the original fillings. It appears certain for Koneprusy and highly probable for Mladec that the fossils fell in through the chimneys. This does not mean that living animals and humans never entered the interior of the caves (traces of gnawing by hyenas are visible), but it makes it unlikely that the human paleontological accumulations were the result of human activity within the cave chambers.     

The pseudoplanktonic crinoid Traumatocrinus from the Late Triassic of Southwest China — Morphology,ontogeny, and taphonomy

The morphology of the pseudoplanktonic crinoid Traumatocrinus from the early Late Triassic (Carnian) Xiaowa Formation of Guanling County (South China, Guizhou Province) is described based on articulated and disarticulated material. Juvenile individuals of less than 10 mm crown height with 20 isotomously branching arms prove the encrinid ancestry of the family Traumatocrinidae. However, even the smallest individuals have five large interradials. Endotomous branching commences at crowns of slightly more than 10 mm at the outer arms of the rays. All brachial articulations are ligamentary (granosyzygies). The assignment of the Chinese material to one of the nominal species of Traumatocrinus is still left open. The diagnosis of the genus Traumatocrinus is emended. Traumatocrinus lived attached to driftwood and was widespread across the Palaeo-Tethys. In contrast to its benthic encrinid ancestors, Traumatocrinus fixed its distal column with countless anastomosing radicular cirri to its substrate, preferentially to the ends of the driftwood logs. Depending on the state of the hypothesized mutable collagene tissue, the columns are preserved in straight positions or curved like a rope. Crowns are preserved in star position with radially splayed arms or in lateral bell position with the cup disrupted in interbrachial position. As usual in black shales, the exposed upper sides of the crinoids are in a more or less progressive state of decomposition whereas the embedded lower sides are intact.     

The spliceosome: a ribozyme at heart?

The spliceosome, the multi-megadalton molecular machine that performs splicing, consists of over 200 different proteins and five small nuclear RNAs (snRNAs). Extensive mechanistic and structural similarities to self-splicing group II introns, large ribozymes found in prokaryotes and lower eukaryotes that catalyze an identical reaction, strongly suggest that the spliceosomal RNAs are in fact the catalytic components of the spliceosome. Of the five spliceosomal RNAs, U2 and U6 are the only ones that are absolutely required for both steps of splicing. These two snRNAs form an elaborate base-paired complex that might in fact constitute the active site of the spliceosome.     

Forest and population at Península de Osa,Costa Rica

The research is focused on the relationship between population growth and conservation of the forest on the Osa Peninsula. Data of the geo-referenced censuses and information on land-use, derived from satellite images and aerial photography, were integrated into a GIS. We undertook an historical inventory of the changes in the population and the forest coverage, and the key events in the land tenure and economy of the region. Deforestation, reforestation, and fragmentation of the forest during the period 1980-1995 were analyzed. Relationships with the population potential, derived from the 1984 Costa Rican censuses, were identified, and the effects of third variables were controlled such as distances to the roads, rain, distances to the forest frontier, level of protection, etc. Both strong and significant associations between 1984 population potential and the three processes were detected. The probability of deforestation is null in unpopulated areas, 35% in areas with 25-30 potential farmers and to 65% in areas with 50 farmers and over. The probability of reforestation decreases from 100% to 28% and to 18% in these three categories. This kind of relationship persists in the multivariable analysis. An increase of 0.63% in the number of household, results in an increment of 1% in the risk of deforestation (elasticity). The elasticity in the chances of reforestation is -0.37 and 1% in fragmentation of the forest. An evaluation in the risk of deforestation for the period 1995-2005 was done. The most recent population data were used and it identifies several geographic areas with high deforestation risk.     

Costly signaling,ritual and cooperation: evidence from Candomblé, an Afro-Brazilian religion

The apparent wastefulness of religious ritual represents a puzzle for rational choice theorists and evolutionary scholars. In recent years, it has been proposed that such rituals represent costly signals that promote intragroup cooperation precisely because of the effort and resources they require. This hypothesis was tested over the course of a 14-month long ethnographic study in the northeast of Brazil. The research focused on adherents of Candomblé, an African diasporic religion organized in autonomous congregations primarily located in low-income urban areas. Individuals who reported higher levels of religious commitment behaved more generously in a public goods economic game and revealed more instances of provided and received cooperation within their religious community. This suggests that ritual as a costly signaling may effectively predict willingness to cooperate with other group members and that the signaler may accrue benefits in the form of received cooperation. Socioeconomic variables are also shown to mediate religious signaling. This raises the possibility that signalers strategically alter their expressions of commitment as their needs and circumstances change.     

The redefinition of Cladiopsocus (Psocoptera: Cladíopsocidae)

The genus Cladiopsocus Roesler is redefined. Seven new species from Central and South America and seven previously described species of Triplocania Roesler are placed in this genus.     

Detecting biodiversity hotspots using species–area and endemics–area relationships: the case of butterflies

Using data of the Red Data Book of European Butterflies we establish the species–area relationship (S = 8.5 A^0.23) and the endemics–area relationship (S = 0.5 A^0.18) of European butterflies. Applying confidence limits as tools for the identification of hotspot countries we show that in the case of butterflies hotspots of endemism and hotspots of overall species richness do not coincide. We introduce plots of residuals from species–area relationships shifted upwards by the 95% confidence limits of the intercept (α-values) as a new tool for identifying and ranking of hotspots.     

An updated assessment of the seabird populations breeding at Príncipe and Tinhosas

The Príncipe Autonomous Region is recognised as a marine biodiversity hotspot, although little is known about the status of its marine fauna. It holds most breeding seabirds of the tropical eastern Atlantic Ocean. Based on anecdotal accounts of increased fishing and seabird harvesting, regular monitoring of seabird populations is considered a priority. Therefore, a survey of Príncipe’s seabird colonies was conducted in 2017. The results revealed that the more accessible seabird colonies have disappeared. Around Príncipe, Boné de Joquei is the present main stronghold for Brown Boobies Sula leucogaster and White-tailed Tropicbirds Phaethon lepturus. The Tinhosas islands hold an estimated 300 000 seabirds, predominantly Sooty Terns Onychoprion fuscatus, but also Brown Boobies, Black Noddies Anous minutus and Brown Noddies Anous stolidus. Long-term multi-annual monitoring is needed to understand the breeding phenology of each species and to better assess population trends. Ensuring a protective status for both Tinhosas and the seabirds under national legislation is a key priority for future conservation policy in São Tomé and Príncipe.     

Palaeoecological studies at the Kaliakra area, northeastern Bulgarian Black Sea coast: 6000?years of natural and anthropogenic change

A 7.5 m sediment core from Lake Bolata, a small former coastal liman lake in northeastern Bulgaria, was analyzed for pollen and plant macrofossil content in attempt to trace the changes in the vegetation, human impact and the influence of the Black Sea during the last ca. 6,000 years. Lake Bolata started its existence when the rising Black Sea level reached the elevation of the bottom of the depression. By that time nearly all tree species were already present in this area with the exception of Carpinus orientalis. The comparison of the arrival time of oriental hornbeam at different sites along the Bulgarian Black Sea confirmed the reliability of the local radiocarbon chronology. For the period under study the vegetation of the region around the site can be described as a forest-steppe due to NAP values higher than 40% of the pollen sum. Forests on the slopes of the river canyon consisted of Quercus spp., Acer, Carpinus orientalis, Fraxinus ornus, Fagus and possibly Tilia. Riverine forests formed stands composed of Salix, Alnus, Ulmus, Fraxinus, Carpinus betulus and Vitis as a liana. The vegetation on the Cape Kaliakra plateau, bordering the canyon, was dominated by diverse herbs and most of these could be considered xerophytes. The oldest occupation period belongs to the Eneolithic, documented by the occurrences of Triticum-type pollen at 5570–5170 cal b.p. (3620–3220 b.c.). The next period of higher continuous Cerealia-type values corresponds to 3450–1830 cal b.p. (1500 b.c.–a.d. 120). The macrofossil record chiefly provides evidence about plant communities of aquatics and helophytes.     

The bacterial diversity on steam vents from Paricutín and Sapichu volcanoes

Extremophiles - Vapor steam vents are prevailing structures on geothermal sites in which local geochemical conditions allow the development of extremophilic microorganisms. We describe the...     

Farming,fishing, and fire in the history of the upper Río Negro region of Venezuela

Studies of Río Negro subsistence farming and fishing activities are used to estimate the human carrying capacity for the region and the likely pattern of human land-use during prehistory. Ceramic evidence suggests human presence in the region more than 3000 years ago. Traditional farming is labor intensive and relatively unproductive. Nevertheless, farmers achieve an energy return of 15.21, and produce 2600 kcal per work hour. Fish are the major protein source, but fish catch per unit of effort and fish yield per hectare of floodplain are very low; fishermen are probably exploiting local fish resources very close to their limit. The low human population density would suggest that the Río Negro forest has been relatively undisturbed. Nevertheless, charcoal is widespread and abundant in forest soils. This charcoal is probably from anthropogenic or natural wildfires. These results suggest a much more complex history for Amazonia than previously thought.K. Clark is a free-lance biologist residing in Lima, Peru