16 research outputs found
The 4.2 ka BP Event in the Mediterranean region: an overview
The Mediterranean region and the Levant have returned some of the clearest evidence of a climatically dry period occurring around 4200 years ago. However, some regional evidence is controversial and contradictory, and issues remain regarding timing, progression, and regional articulation of this event. In this paper, we review the evidence from selected proxies (sea-surface temperature, precipitation, and temperature reconstructed from pollen, δ18O on speleothems, and δ18O on lacustrine carbonate) over the Mediterranean Basin to infer possible regional climate patterns during the interval between 4.3 and 3.8 ka. The values and limitations of these proxies are discussed, and their potential for furnishing information on seasonality is also explored. Despite the chronological uncertainties, which are the main limitations for disentangling details of the climatic conditions, the data suggest that winter over the Mediterranean involved drier conditions, in addition to already dry summers. However, some exceptions to this prevail - where wetter conditions seem to have persisted - suggesting regional heterogeneity in climate patterns. Temperature data, even if sparse, also suggest a cooling anomaly, even if this is not uniform. The most common paradigm to interpret the precipitation regime in the Mediterranean - a North Atlantic Oscillation-like pattern - is not completely satisfactory to interpret the selected data
Psyllium husk gel to reinforce structure of gluten-free pasta?
Gluten-free pasta is a technological challenge. The effect of Psyllium particle size, processing temperature and gel
concentration on the quality of rice-based pasta was investigated. The rheological properties, i.e. maturation
kinetics and mechanical spectra, of the Psyllium gels were studied and optimal conditions were set: 160–315 μm
particle size, 4 g/100 g Psyllium husk concentration thermally processed at 40 ºC. Cooking quality parameters,
texture properties, nutritional composition, antioxidants and digestibility of pasta were determined. Consequently,
the use of Psyllium husk in gluten-free pasta showed good overall properties. Moreover, the pregelatinization
step of rice flour can be eliminated, resulting in a final gluten-free pasta formulation with Psyllium
gel and rice flour (50/50) with high digestibilityinfo:eu-repo/semantics/publishedVersio
Genome sequence of the tsetse fly (Glossina morsitans):Vector of African trypanosomiasis
Tsetse flies are the sole vectors of human African trypanosomiasis throughout sub-Saharan Africa.
Both sexes of adult tsetse feed exclusively on blood and contribute to disease transmission. Notable
differences between tsetse and other disease vectors include obligate microbial symbioses, viviparous
reproduction, and lactation. Here, we describe the sequence and annotation of the 366-megabase
Glossina morsitans morsitans genome. Analysis of the genome and the 12,308 predicted
protein-encoding genes led to multiple discoveries, including chromosomal integrations of bacterial
(Wolbachia) genome sequences, a family of lactation-specific proteins, reduced complement of
host pathogen recognition proteins, and reduced olfaction/chemosensory associated genes. These
genome data provide a foundation for research into trypanosomiasis prevention and yield important
insights with broad implications for multiple aspects of tsetse biology.IS
The 4.2 ka BP Event in the Mediterranean region: an overview
International audienceThe Mediterranean region and the Levant have returned some of the clearest evidence of a climatically dry period occurring around 4200 years ago. However, some regional evidence is controversial and contradictory, and issues remain regarding timing, progression, and regional ar-ticulation of this event. In this paper, we review the evidence from selected proxies (sea-surface temperature, precipitation , and temperature reconstructed from pollen, δ 18 O on speleothems, and δ 18 O on lacustrine carbonate) over the Mediterranean Basin to infer possible regional climate patterns during the interval between 4.3 and 3.8 ka. The values and limitations of these proxies are discussed, and their potential for furnishing information on seasonality is also explored. Despite the chronological uncertainties, which are the main limitations for disentangling details of the climatic conditions , the data suggest that winter over the Mediterranean involved drier conditions, in addition to already dry summers. However, some exceptions to this prevail-where wetter conditions seem to have persisted-suggesting regional heterogeneity in climate patterns. Temperature data, even if sparse, also suggest a cooling anomaly, even if this is not uniform. The most common paradigm to interpret the precipitation regime in the Mediterranean-a North Atlantic Oscillation-like pattern-is not completely satisfactory to interpret the selected data