Sedimentary archives of climate and sea-level changes during the Holocene in the Rhone prodelta (NW Mediterranean Sea)

A 7.38 m-long sediment core was collected from the eastern part of the Rhone prodelta (NW Mediterranean) at 67 m water depth. A multi-proxy study (sedimentary facies, benthic foraminifera and ostracods, clay mineralogy, and major elements from XRF) provides a multi-decadal to century-scale record of climate and sea-level changes during the Holocene. The early Holocene is marked by alternative silt and clay layers interpreted as distal tempestites deposited in a context of rising sea level. This interval contains shallow infra-littoral benthic meiofauna (e.g. Pontocythere elongata, Elphidium spp., Quinqueloculina lata) and formed between ca. 20 and 50 m water depth. The middle Holocene (ca. 8.3 to 4.5 ka cal. BP), is characterized, at the core site, by a period of sediment starvation (accumulation rate of ca. 0.01 cm yr−1) resulting from the maximum landward shift of the shoreline and the Rhone outlet(s). From a sequence stratigraphic point of view, this condensed interval, about 35 cm-thick, is a Maximum Flooding Surface that can be identified on seismic profiles as the transition between delta retrogradation and delta progradation. It is marked by very distinct changes in all proxy records. Following the stabilization of the global sea level, the late Holocene is marked by the establishment of prodeltaic conditions at the core site, as shown by the lithofacies and by the presence of benthic meiofauna typical of the modern Rhone prodelta (e.g. Valvulineria bradyana, Cassidulina carinata, Bulimina marginata). Several periods of increased fluvial discharge are also emphasized by the presence of species commonly found in brackish and shallow water environments (e.g. Leptocythere). Some of these periods correspond to the multi-decadal to centennial late Holocene humid periods recognized in Europe (i.e. the 2.8 ka event and the Little Ice Age). Two other periods of increased runoffs at ca. 1.3 and 1.1 ka cal. BP are recognized, and are likely to reflect periods of regional climate deterioration that are observed in the Rhone watershed.

Degradación ambiental y conflictos armados: las conexiones

"La seguridad ambiental es un concepto complejo que puede ser analizado desde varios enfoques. La conexión entre degradación ambiental, escasez de recursos, poco desarrollo económico e inestabilidad política puede generar rápidamente conflictos llamados ambientales, terrorismo ecológico y guerras verdes. Sin embargo, en la mayoría de las investigaciones sobre degradación ambiental y conflictos armados no se tienen en cuenta los factores desarrollo económico y régimen político, pues se considera que los problemas ambientales pueden, por sí solos, conducir a situaciones conflictivas nacionales, regionales e internacionales. En este contexto, los propósitos de este artículo son plantear las diferentes tendencias ideológicas de la seguridad ambiental, definir el contenido y las causas de los conflictos ambientales y proponer un marco analítico complementario que incluya las variables políticas y económicas como generadoras de conflictos ambientales y de conflictos armados de alta intensidad. Al final, se propone una agenda de investigación en materia de seguridad ambiental para Colombia."

Biomarker analysis in soils of the Amazon rainforest after vegetation fire.

The objective of this study was to determine the origin of organic matter incorporated in Amazon forest soils subjected to vegetation fire by analyzing the aliphatic biomarkers (n-alkanes) present in lipid extracts of soil samples.