LATE CARBONIFEROUS BRACHIOPODS FROM KARAKORUM, PAKISTAN

Carboniferous rocks from North Karakorum display sharp lateral variations in lithology and thickness suggesting accumulation in half-grabens during continental rifting between the Karakorum block and northern Gondwana. Different Carboniferous successions, belonging to distinct tectonic units, have been detected. Thin, poorly fossiliferous successions of arenites and crinoidal limestones contrast with very thick terrigenous-carbonate successions comprising two distinct fossiliferous horizons. The lower fossiliferous horizon yielded brachiopods (Pustula sp., Rhipidomella sp., Choristites sp., Martiniopsis sp., Afghanospirifer sp., Gypospirifer sp., Composita sp.) of Bashkirian age. The upper fossiliferous horizon, lying about 90 m above the former, contains corals, crinoids and brachiopods (Densepustula cf. losarensis, Dowhatania sulcata n. sp., Brachythyris sp., Rhipidomella sp., Septacamera dowhatensis, Alispirifer middlemissi) of Moscovian to Kasimovian age. The Carboniferous brachiopods of North Karakorum are similar to those collected in the Late Carboniferous of Central Afghanistan, Himalaya (Manang, Spiti, Tibet), and Lhasa Block (Xainza area).&nbsp

Precollisional development and Cenozoic evolution of the Southalpine retrobelt (European Alps)

The retrobelts of doubly vergent collisional orogens are classically interpreted as late-stage postcollisional features. Here, we integrate literature data with new structural and thermochronological evidence from the European Alps in order to document the precollisional development of the retrobelt segment exposed in the central southern Alps. During the Late Cretaceous, by inversion of inherited extensional faults of Permian age, the Variscan basement of the central southern Alps was stacked southward onto the Permian-Mesozoic cover sequences of the Adria margin. These thrust systems were first deformed within regional-scale antiforms (the "Orobic anticlines") and then cut by Eocene magmatic bodies. Our apatite fission-track data show that these units were largely structured and exhumed to shallow crustal levels before the intrusion of the Eocene magmatic rocks. Therefore, thrusting and folding in the Alpine retrobelt took place before the final closure of the Alpine Tethys and subsequent continental collision between Adria and Europe. Final exhumation and uplift in the northern part of the Southalpine retrobelt took place under a dextral transpressional regime largely coeval with the right-lateral strike-slip activity along the Insubric fault. In Neogene times, deformation propagated southward, leading to the formation of a frontal thrust belt that is largely buried beneath the Po Plain

Age and isotopic constraints on magmatism along the Karakoram-Kohistan Suture Zone, NW Pakistan: evidence for subduction and continued convergence after India-Asia collision

Abstract.: Detailed geological mapping in the Drosh-Shishi area in southern Chitral (NW Pakistan) was combined with high-precision U-Pb dating on zircons to constrain the timing of magmatism and associated deformation/metamorphic events related to the Kohistan-Karakoram convergence and collision. Our new ages indicate that the Mesozoic to Tertiary magmatic history of this region is influenced by long-lived melt generation above an active subduction zone. Dated intrusive rocks range in age from 130 to 39 million years, indicating that subduction-related magmatism continued after the Kohistan-Karakoram and the India-Asia collisions. Initial hafnium isotope ratios were measured on the dated zircons to constrain the type of melt source of the dated plutons. The data reveal the different nature of partly coeval magmatism in these units, i.e. continental arc magmatism in the Karakoram (ca. 130-104 Ma) and arc magmatism magmatism on the Kohistan side (112-39 Ma). Intrusions within the suture zone can be clearly traced to be Karakoram-derived on the basis of initial Hf isotopic compositions. Granite dykes crosscutting the Kohistan units have sampled an underlying, old continental basement of Gondwana affinity. The geochronological evidence presented in this paper is consistent with Cretaceous subduction beneath the Karakoram Terrane. The related calc-alkaline magmatism seems to have stopped at about 100 Ma. Granite dykes on the Kohistan side show that the magmatic and tectonic history of the Karakoram-Kohistan Suture Zone continued to the Eocene. This long tectono-metamorphic and magmatic activity in the arc plates was likely due to complex and few million year long interplays between subduction and thrusting events in the forearc, within-arc and back-arc regions between two active subduction zone

Opening of the Neo-Tethys Ocean and the Pangea B to Pangea A transformation during the Permian

We studied the stratigraphy, composition, and paleomagnetic properties of lateritic weathering profiles of Permian age from northern Iran and western Karakoram, Pakistan. A limited set of samples deemed representative yielded stable low-inclination paleomagnetic components carried essentially by hematite of chemical origin isolated in massive, fine-grained, and homogeneous ferricrete facies. These laterites originated at equatorial paleolatitudes characterized by intense weathering processes under warm and humid climatic conditions. Paleomagnetic estimates of paleolatitude from Iran, Karakoram, and north Tibet from this study and the literature, albeit sparse, provide testable constraints on the motion of the Cimmerian terranes as the result of the opening of the Neo-Tethys Ocean along the eastern margin of Gondwana during the Permian. We confirm and help refine previous suggestions that the Cimmerian terranes migrated from southern Gondwanan paleolatitudes in the Early Permian to subequatorial paleolatitudes by the Middle Permian – Early Triassic. As a novel conclusion, we find that timing, rates, and geometry of Cimmerian tectonics are broadly compatible with the transformation of Pangea from an Irvingian B to a Wegenerian A-type configuration with Neo-Tethyan opening taking place contemporaneously essentially in the Permian

Effetti di tipologie di suolo e colture foraggere sulle perdite per ruscellamento di azoto, fosforo e potassio in differenti areali italiani

Le colture foraggere svolgono un ruolo importante in molti areali italiani. Per una corretta pianificazione del territorio agricolo è necessario approfondire la conoscenza non solo delle caratteristiche produttive di queste colture, ma anche dei loro rapporti con l'ambiente. Questo lavoro prende in considerazione le perdite di azoto, fosforo e potassio dovute al ruscellamento in colture foraggere a diverso livello di intensificazione (dal pascolo alla coltura di erba medica, dal mais al doppio ciclo di mais e loiessa) in tre ambienti italiani: la Pianura Padana nord-occidentale, l'Appennino Toscano e la pianura sarda, con suoli varianti da franco-sabbioso a franco-argilloso. Il monitoraggio quanti-qualitativo del ruscellamento è stato fatto per periodi variabili da due a sei anni. La pendenza era dello 0,5% per gli appezzamenti in Piemonte e Sardegna e del 10% in Toscana. Per quanto riguarda l'azoto i rilasci sono risultati più bassi nei terreni più pianeggianti, anche per i ridotti volumi di ruscellamento registrati, non superando mai 15 kg di N ha -1 anno -1. Nei terreni in pendenza si sono invece registrati valori più elevati, con un massimo annuale di circa 30 kg ha -1 anno -1 di azoto, in relazione anche all'elevato ruscellamento ed erosione di un evento eccezionale. Per il fosforo solo in pochi casi si sono raggiunte perdite di 5 kg ha -1 anno -1, mentre nella maggior parte dei casi non sono stati superati 2 kg ha -1 anno -1. In Sardegna i rilasci di tale elemento sono da considerarsi pressoché trascurabili. Le perdite di potassio sono risultate minime in Sardegna e massime in Piemonte, dove si sono registrati valori dell' ordine di 10 kg ha -1 anno -1. Ove era possibile il confronto, si è verificato che le colture prative riducono il rilascio di elementi nutritivi rispetto alla coltura del mais e che la qualità delle acque di superficie appare legata piuttosto alle tecniche colturali che alla tipologia di suolo. Fodder crops play an important role in many Italian environments. The knowledge of the main productive characteristics of these crops is as important as their relationships with the environment, expecially for a proper territorial management. This paper compares nitrogen, phosphorous and potassium contents in runoff of some forage crops of different intensity (pasture, lucerne, silage maize, Italian ryegrass/maize double cropping) in different ltalian environments (north-western plain of Piemonte, Apennines hills of Tuscany and Mediterranean plain of Sardegna) on different typology of soils. Runoff data have been collected for periods ranging between two and six year, from plots of different extension and slope (0,5% in the plains, 10% in Apennine hills). Nitrogen losses, for the small amount of runoff, have been qui te low from ilat fields, being always less than 15 kg ha -1 year-1. Losses from slope fields have been higher, with a maximum of 30 kg ha -1 year-1, due to very high level of runoff and erosion in a conspicuous episode. Phosphorous losses only in a few cases were higher than 5 kg ha -I year -I, while mostly they have b>!en less than 2 kg ha -1 year-1. In the Mediterranean plain such losses have been quite insignificant. Minimum potassium 10sses were recorded in the Mediterranean plain, while in north-western plain they reached about 10 kg-1 year-1. Maize was, on average, the crop with highest nutrient losses, while quality of the runoff water was more related to agricultural practices than to soil types

Modellizzazione della lisciviazione dei nitrati: calibrazione e validazione del modello LEACHN in diversi suoli e colture foraggere

The LEACHN model calibration and validation was realized in three Italian enviroments (Piedmont, Tuscany and Sardinia), using nitrate losses by drainage from 4 soil types ranging from sandy-loam to day-loam. A set of large drainage lysimeters were used to obtain leaching data. In each location one lysimeter was cultivated with lucerne, while the others were cropped with widespread crops in the area (maize for silage in Piedmont and Sardinia and permanent pasture in Tuscany). Measured leaching losses ranged from l to 68 kg ha-1 year-1. The calibration parameters were humus mineralization rate and nitrification rate. The calibration was realized on a not nitrogen fixing crop, while the validation was executed on lucerne, even if there is not a specific N-fixation subroutine in LEACHN. After calibration, the prediction of nitrate losses cumulated over the whole period (two years) or over each month resulted acceptable for all crops, while the single event prediction was totally inadequate. The LEACHN model seems to be applicable for the nitrate leaching prediction on a territorial scale. In tre areali italiani (pianura piemontese, conca interappenninica toscana, pianura irrigua sarda) e su quattro diversi tipi di terreno si è calibrato e validato il modello LEACHN relativamente alla previsione della lisciviazione dei nitrati. Si è operato con lisimetri a drenaggio di grandi dimensioni. In tutte le situazioni un lisimetro era coltivato a erba medica, mentre altri con colture di ampia diffusione nell'arcale: mais da trinciato integrale in Piemonte, doppio ciclo colturale di loiessa e mais da granella in Sardegna e pascolo in Toscana e Sardegna. Le perdite per lisciviazione misurate sono risultate comprese tra l e 68 kg ha-1 anno-1 di NO-3-N. Come parametri di calibrazione si sono usati il tasso di mineralizzazione dell'humus e il tasso di nitrificazione dello ione ammonio, calibrati sulla coltura non azotofissatrice. Sull'erba medica, per la quale non è prevista alcuna routine per l'azotofissazione, è stata invece condotta la validazione. Dopo la calibrazione, la simulazione della lisciviazione cumulata e dei totali mensili lisciviati è risultata accettatile, anche su erba medica, mentre quella dei singoli eventi è stata del tutto insufficiente. Il modello nel complesso è apparso applicabile per la predizione delle perdite di nitrati anche su scala territoriale

Evolution of macrolide resistance in streptococcus pyogenes over 14 years in an area of central Italy

We evaluated temporal fluctuations in macrolide resistance rates, analysing genetic determinants of resistance and clonal evolution in a population of 2744 S. pyogenes isolates collected in the period 2000–2013. The total resistance rate to erythromycin of the isolates was 17.9%. A maximum of erythromycin resistance emerged in 2000 (38.6%), followed by a significant decrease to 5.2% in 2012 (P<0.0001). Molecular analysis revealed the presence and co-presence of known genetic resistance determinants mefA, mefE, ermTR and ermB, in line with phenotypes. PFGE analysis identified genetically related groups in 2000 and 2007–2008, mainly the MLS and M phenotypes, respectively. The most prevalent emm types among a representative subset of resistant isolates were emm2, emm75 and emm77. All emm2 and 88.2% of the strains harbouring the emm75 gene were only recorded in M-phenotype strains, whilst all emm77-positive strains had the inducible MLS phenotype. The analysed susceptible isolates showed several emm types partially shared with resistant ones. Our results suggest that changes in bacterial population clonality, rather than horizontal transfer of resistance determinants, plays a major epidemiological role in S. pyogenes. Continuous monitoring of microbiological epidemiology seems to be crucial for correct and effective management of streptococcal infections

OLENEKIAN TO EARLY LADINIAN STRATIGRAPHY OF THE WESTERN PART OF THE AGHDARBAND WINDOW (KOPEH-DAG, NE IRAN)

The structural setting and the stratigraphy of the Early to Middle Triassic sedimentary succession exposed in the western part of the Aghdarband window (Kopeh Dag, NE Iran) is described. Six stratigraphic sections in the Sefid-Kuh Limestone, Nazar-Kardeh Formation and Sina Formation have been studied in the tectonic units 1a and 2. The lithostratigraphy is revised, with bio-chronostratigraphic constrain provided by conodonts and ammonoids. The new Olenekian ammonoid genus Megatirolitesis erected. It is based on species thus far known only in Mangyshlak (West Kazakhstan) but it is occurs also in the Sefid-Kuh Limestone.The evolution of the Lower Triassic carbonate ramp of the Sefid-Kuh Limestone, persisted in the Middle Anisian, with a three-stage development (Sefid-Kuh 1, 2 and 3 members) separated by drowning and onset of siliciclastics. The last stage is in part coeval with the Middle Anisian basinal Nazarkardeh Formation.The unconformity-bounded, three-stage development of the carbonate ramp documents that in the Aghdarband Basin the tectonic control over sedimentation started already in the Olenekian, since the onset of the marine transgression. The transgression of the Ladinian Sina Formation sealed a complex morphology resulting from the uplift and erosion of the Middle Anisian units. A new paleogeographic position along the southern Laurasia margin is propsed for the Triassic Aghdarband Basin. Based on the paleobiogeographic affinity of the Olenekian ammonoid occurences, we suggest that the Aghdarband Basin was located in a back-arc position in close connection with Mangyshlak (West Kazakhstan) and Tuarkyr (Turkmenistan), passing northwestward to a large epicontinental basin extending to the Donbass area. At least during the Olenekian the Aghdarband Basin had no direct connection with the Nakhlak Basin, which was proably located in a different intra-arc or more probably fore-arc region with respect to the Palaeotethys subduction-related Triassic arc