New earwig nymphs (Dermaptera: Pygidicranidae) in mid-Cretaceous amber from France

A new genus and species of earwig is described and figured from Early Cretaceous (Latest Albian-Earliest Cenomanian) amber of southwestern France. The holotype was studied using traditional light microscopy as well as through propagation phase contrast X-ray synchrotron microtomography, rendering high resolution three-dimensional models for critical examination. Gallinympha walleri Perrichot & Engel, new genus and species, is represented by two late instar nymphs missing only portions of the abdomen, as well as most of the head for the paratype. The genus is a member of the Pygidicranidae, one of the most basal of living earwigs, and is distinguished from other taxa in the family. A thorough account of the specimen’s morphology is provided along with a detailed comparison with similar structures across a diversity of primitive earwig lineages.     

Investigation of groundwater mineralization in the Hammamet–Nabeul unconfined aquifer,north-eastern Tunisia: geochemical and isotopic approach

Detailed hydrogeochemical and isotopic data of groundwaters from the Hammamet–Nabeul unconfined aquifer are used to provide a better understanding of the natural and anthropogenic processes that control the groundwater mineralization as well as the sources of different groundwater bodies. It has been demonstrated that groundwaters, which show Na–Cl and Ca–SO₄–Cl water facies, are mainly influenced by the dissolution of evaporates, the dedolomitization and the cation-exchange process; and supplementary by anthropogenic process in relation with return flow of irrigation waters. The isotopic signatures permit to classify the studied groundwaters into two different groups. Non-evaporated groundwaters that are characterized by depleted δ ¹⁸O and δ ²H contents highlighting the importance of modern recharge at higher altitude. Evaporated groundwaters with enriched contents reflecting the significance infiltration of return flow irrigation waters. Tritium data in the studied groundwaters lend support to the existence of pre-1950 and post-1960 recharge. Carbon-14 activities in shallow wells that provide evidence to the large contamination by organic ¹⁴C corroborate the recent origin of the groundwaters in the study area.     

Quenching of phosphorus fixation with organic wastes in a bauxite mine overburden

Capabilities of two phosphate-rich organic wastes to quench phosphorus (P) fixation in a stored high-phosphorus-fixing tropical bauxite overburden were examined in a field experiment. Prior grinding and ensiling of shrimp shell waste facilitated increased solubility and hence phosphorus fixation quenching in the soil. Normal plant-available P concentrations were exhibited by the overburden for up to 4 months after application despite the cultivation and harvesting of plants in the treated beds. Ten-year-old, stored overburden treated with ensiled shrimp shell silage, or chicken manure exhibited P levels of 1.0 and 1.1%, respectively, 4 months after treatment application. This represents a small excess over normal concentrations of free P in the overburdens. These P levels dropped to 0.055 and 0.060%, respectively, after 8 months. The capacity of the soil to fix phosphorus was thus rapidly “filled” with an excess of P in the overburden. However, increased P fixation in the second 4-month period was attributed to the inherently high levels of Ca²⁺ in the ground. Therefore, amelioration based on quarterly applications promises a long-term corrective for P-fixing in stored bauxite overburdens.     

Freshwater seepages and ephemeral macroalgae proliferation in an intertidal bay: I Effect on benthic community structure and food web

Freshwater seepages and ephemeral Enteromorpha spp. proliferation create heterogeneity at small spatial scale in intertidal sediment. Macrobenthic community diversity was compared between these two disturbances and their respective control points throughout the year 2007 at the Roscoff Aber Bay (Western English Channel, France). In March and September 2007, trophic community pathways of characteristic species were additionally studied using stable isotope ratios of carbon and nitrogen. The low salinity recorded at the freshwater seepage induced the exclusion of the main bioturbator and the presence of omnivores which modified the community composition by biotic pressure. Moreover, food web analyses clearly highlighted a separation at small spatial scale between the two trophic pathways of the impacted area and its control. On the contrary, little differences were observed owning to the ephemeral Enteromorpha spp. proliferation. This suggested a progressive and diffusive disturbance which was applied from the algal mat to the nearby area. However, seasonal changes were observed. First, the algal expansion phase increased the macrofauna diversity and foraminifers’ abundance (meiofauna) and then acted as a physical barrier decreasing sediment and water column exchanges and decreasing the fauna diversity. This study highlights the need to take into account small spatial heterogeneity to avoid misinterpretations in intertidal ecology studies.     

The Sis palaeovalley: a record of proximal fluvial sedimentation and drainage basin development in response to Pyrenean mountain building

The Sis conglomerate body represents the Middle Eocene to Oligocene transfer‐zone trunk palaeovalley fill of the Sis fluvial system, a drainage system established within the Pyrenees during Late Palaeocene times. The spatial stability of the fluvial transfer zone (active for at least 38 My), and hence the longevity of its aggradational palaeovalley component (>19·5 My), was controlled by its location between long‐lived pre‐existing structures. Coarse‐grained fluvial facies dominate the palaeovalley fill, with alluvial fan facies shed from its defining marginal structures. The detailed sedimentology of very proximal fluvial facies deposited within the dominantly erosional realm of an active mountain belt has rarely been documented before because of their poor preservation potential. The Sis conglomerate body contains a robust internal stratigraphy with stratigraphic units defined by distinct bounding surfaces, across which there are pronounced changes in facies and provenance. These mark the reorganization of the headward portions of the Sis fluvial system during the evolution of the Pyrenean Axial Zone antiformal stack. Major changes in discharge resulted, demonstrating the highly variable nature of even mountain belt‐scale fluvial systems when viewed on timescales of several to tens of millions of years. Provenance details indicate that initial unroofing of Hercynian granitoids, situated within the Pyrenean Axial Zone, occurred around 54·5 Ma (early Ypresian) immediately before the first significant exhumation event within the drainage basin of the Sis fluvial system. This is earlier than previously constrained by apatite fission track studies. Rock uplift accelerated in the Lutetian and Bartonian with the initial aggradation of the palaeovalley fill (the Cajigar and Cornudella Formations and Sis One and Two Members). This became marked in the Priabonian (Sis Three and Four Members), with significant activity on local structures including the Morreres backthrust. An increase in basement‐derived clasts and a headwater decapitation event also indicate pronounced Axial Zone antiformal stack development at this time. Axial Zone development intensified further in the Oligocene with the deposition of the Collegats Formation and the switch in the main depositional loci of the system from the Tremp‐Graus thrust‐sheet‐top basin to the Ebro Basin to the south.     

The 1928–1929 eruption of Kammourta volcano — evidence of tectono-magmatic activity in the Manda-Inakir rift and comparison with the Asal Rift,Afar depression,Republic of Djibuti

There are two rifts zones in the Republic of Djibuti: the active Asal rift (birthplace of the Ardoukôba basaltic volcano in 1978) and the poorly known Manda-Inakir rift described here. The most recent volcanic event in the Manda-Inakir rift was the formation of the Kammourta basaltic cone, probably in 1928, accompanied by strong seismic activity. This historic eruption and related tectonic features show that the Manda-Inakir rift, like Asal, is presently active. The Kammourta basalt, of transitional alkaline type, belongs to the Manda-Inakir differentiated series, which ranges from basalt to rhyolite. In contrast, volcanic rocks of the Asal rift are entirely transitional tholeiitic basalt. The differences in magmatic affinity and tectonics between these two rift zones reflect the more advanced evolution of rifting in the Asal zone than in Manda-Inakir.     

Effects of heterogeneous land use/cover types on river channel morphology in the Solo River catchment,Eastern Uganda

In the tropics, unmonitored land use/cover types cause significant effects on the narrowing and widening of river channels which affects the integrity of water resources. River channel planform extent was characterized using Landsat images, while water and bedload samples were collected and analysed for a period of one year. The results revealed that in 1986, the channel planform covered 3.7 sq km in length than in 2013 where it increased to 4.2 sq km. Wetland (537.1mgl^?1) and bushland (186.3mgl^?1) cover types had the highest concentration of suspended sediments. Fine sand (0.25 mm), silty sand (1 mm) and silty clay (0.125 mm) bedload particle types dominated the riverbed along the channel from the sampled land use/cover types. The high concentration of sediments, bedload materials, bank instability, and streamflow were significant contributors to the narrowing and widening of the channel (p < 0.05). Agricultural land use was the major contributor of channel aggradation (0.8 m) and degradation (0.25 m) compared to tree plantations, bushlands, forest and wetland cover types.     

High altitude aircraft remote sensing during the 1988 Yellowstone national park wildfires

Abstract

The advancement of satellite remote sensing has offered greater potential for mapping volcanic deposits. Although the development of weather‐independent microwave remote sensing has made the frequent detection over large area detection of deposits using SAR intensity image is sometimes hindered by ambiguities and noise. The ambiguities occur in volcanic deposit areas covered by young vegetation and that give either high or low backscatter depending upon their orientation. For this reason coherent images were integrated with SAR intensity images to extract more reliable information about volcanic deposited area. Besides, the layover areas due to the viewing geometry of SAR make difficulties to map the volcanic deposits on every side of the mountain. To avoid the influence of layover effects fusion techniques of ascending and descending pass SAR intensity and coherent images were developed. Using the fused images with an optical image, a color composite was developed to identify the areas affected by an eruption. In this color composite, especially vegetation damages can be easily identified.     

A GIS‐based Vehicle Mobility Estimator for Operational Contexts

A vehicle mobility estimator has been developed to produce decision aid maps for projecting civil or military forces on operational theatres. Based on the exploitation of classical geographical sources (e.g. digital elevation models, optical images, and vector databases) and thematic sources (e.g. climate, meteorological, pedological and land cover databases), the system computes speed maps for different kinds of vehicles moving both on‐road and off‐road. Such computations are realized through a ground‐vehicle interaction module that estimates the vehicle performance from experimental results, numerical simulations and empirical relationships. The system's architecture is built using a GIS interface that manages the data, the computation and the presentation layers. An operational version of this tool has been tested and validated on several operational theatres in France and in northern Africa. The results show good agreement between the predicted mobility performance of various vehicles and those observed on the field. A case study is presented to illustrate the mobility maps and demonstrate their relevance in the decision‐making chain depending on different climate contexts. A short application to itinerary optimization is presented as a promising future application.     

The Indigenous Aetas of Bataan,Philippines: Extraordinary genetic origins,modern history and land rights

The Aeta Magbukún of Bataan in Luzon, the Philippines remain one of the least known and documented Indigenous tribes. They retain primarily subsistence hunter‐gathering strategies to supply their basic needs. They also strive for recognition of their ancestral connection with, and rights to inhabit their ancestral forest domains, which is threatened by the expansion of agriculture and urban development by non‐Aetas, primarily the majority Tagalog population. The Aeta continue to endure dispossession, poverty and political discrimination through decades of protracted land rights processes. This review explores the potential use of recent genetic evidence in anthropology and human geography to legitimize the Aeta's status as Indigenous people and contradict the perspective of some governments in the Asia Pacific region who question the existence of Indigenous peoples generally, often from fear of land tenure and associated political repercussions. The acquisition and use of genetic research on Indigenous populations is both socially and politically contested through fear of the potential to jeopardize sovereignty claims and lead to biologically‐based discrimination. However, the full implications of the potential use of genetic research to legitimize Indigenous status, as described within this research, has yet to be thoroughly explored. By exploring both the genetic and anthropological evidence using a case study of the Indigenous Aeta, this paper provides a unique approach to building a case for Indigenous rights, occupation, use of ancestral lands, self‐determination, and ultimately, recognition as Indigenous people.