High-resolution multi-proxy record of the last glacial period from Lake Van, eastern Anatolian high plateau, Turkey

Detailed analyses of the Lake Van pollen, Ca/K ratio and stable oxygen isotope record allow the identification of millennial-scale vegetation and environmental changes in eastern Anatolia throughout the last glacial (~75-15 ka BP). The climate within the last glacial was cold and dry, with low arboreal pollen (AP) levels. The driest and coldest period corresponds to Marine Isotope Stage (MIS) 2 (~28-14.5 ka BP) dominated by the highest values of xerophytic steppe vegetation. Our high-resolution multi proxy record shows rapid expansions and contractions of tree populations that reflects variability in temperature and moisture availability. This rapid vegetation and environmental changes can be linked to the stadial-interstadial pattern of the Dansgaard-Oeschger (DO) events as recorded in the Greenland ice cores. Periods of reduced moisture availability were characterized by enhanced xerophytic species and high terrigenous input from the Lake Van catchment area. Furthermore, comparison with the marine realm reveals that the complex atmosphere-ocean interaction can be explained by the strength and position of the westerlies, which is responsible for the supply of humidity in eastern Anatolia. Influenced by diverse topography of the Lake Van catchment, larger DO interstadials (e.g. DO 19, 17-16, 14, 12 and 8) show the highest expansion of temperate species within the last glacial. However, Heinrich events (HE), characterized by highest concentrations of ice-rafted debris (IRD) in marine sediments, are identified in eastern Anatolia by AP values not lower and high steppe components not more abundant than during DO stadials. In addition, this work is a first attempt to establish a continuous microscopic charcoal record over the last glacial in the Near East, which documents an initial immediate response to millennial-scale climate and environmental variability and enables us to shed light on the history of fire activity during the last glacial.

High-resolution multi-proxy record of the last interglacial period from Lake Van, eastern Anatolian high plateau, Turkey

A high-resolution multi-proxy record from Lake Van, eastern Anatolia, derived from a lacustrine sequence cored at the 357 m deep Ahlat Ridge (AR), allows a comprehensive view of paleoclimate and environmental history in the continental Near East during the last interglacial (LI). We combined paleovegetation (pollen), stable oxygen isotope (d18Obulk) and XRF data from the same sedimentary sequence, showing distinct variations during the period from 135 to 110 ka ago leading into and out of full interglacial conditions. The last interglacial plateau, as defined by the presence of thermophilous steppe-forest communities, lasted ca. 13.5 ka, from ~129.1-115.6 ka BP. The detailed palynological sequence at Lake Van documents a vegetation succession with several climatic phases: (I) the Pistacia zone (ca. 131.2-129.1 ka BP) indicates summer dryness and mild winter conditions during the initial warming, (II) the Quercus-Ulmus zone (ca. 129.1-127.2 ka BP) occurred during warm and humid climate conditions with enhanced evaporation, (III) the Carpinus zone (ca. 127.2-124.1 ka BP) suggest increasingly cooler and wetter conditions, and (IV) the expansion of Pinus at ~124.1 ka BP marks the onset of a colder/drier environment that extended into the interval of global ice growth. Pollen data suggest migration of thermophilous trees from refugial areas at the beginning of the last interglacial. Analogous to the current interglacial, the migration documents a time lag between the onset of climatic amelioration and the establishment of an oak steppe-forest, spanning 2.1 ka. Hence, the major difference between the last interglacial compared to the current interglacial (Holocene) is the abundance of Pinus as well as the decrease of deciduous broad-leaved trees, indicating higher continentality during the last interglacial. Finally, our results demonstrate intra-interglacial variability in the low mid-latitudes and suggest a close connection with the high-frequency climate variability recorded in Greenland ice cores.

Data from the EPICA Dome C ice core EDC

The Antarctic Vostok ice core provided compelling evidence of the nature of climate, and of climate feedbacks, over the past 420,000 years. Marine records suggest that the amplitude of climate variability was smaller before that time, but such records are often poorly resolved. Moreover, it is not possible to infer the abundance of greenhouse gases in the atmosphere from marine records. Here we report the recovery of a deep ice core from Dome C, Antarctica, that provides a climate record for the past 740,000 years. For the four most recent glacial cycles, the data agree well with the record from Vostok. The earlier period, between 740,000 and 430,000 years ago, was characterized by less pronounced warmth in interglacial periods in Antarctica, but a higher proportion of each cycle was spent in the warm mode. The transition from glacial to interglacial conditions about 430,000 years ago (Termination V) resembles the transition into the present interglacial period in terms of the magnitude of change in temperatures and greenhouse gases, but there are significant differences in the patterns of change. The interglacial stage following Termination V was exceptionally long - 28,000 years compared to, for example, the 12,000 years recorded so far in the present interglacial period. Given the similarities between this earlier warm period and today, our results may imply that without human intervention, a climate similar to the present one would extend well into the future.

ST13 polymorphisms and their effect on exacerbations in steroid-treated asthmatic children and young adults

© 2015 John Wiley & Sons Ltd.

Adaptación psicométrica de los cuestionarios "Trauma Symptom Checklist for Children" (TSCC) y "Trauma Symptom Checklist for Young Children" (TSCYC) en una muestra española de víctimas de abuso sexual infantil

El maltrato infantil y el abuso sexual, como tipo de maltrato en la infancia, supone un problema social que ha estado presente a lo largo de la historia, en todos los países, culturas, estratos sociales. El abuso sexual infantil ha presentado dificultades para su definición al no existir un acuerdo único y darse diferencias sobre los criterios definitorios. Las definiciones propuestas han sido múltiples, algunas son más restrictivas, mientras que otras tienen una perspectiva más amplia. Una de las definiciones más ampliamente usada y aceptada internacionalmente ha sido la propuesta por la OMS (2001), al incorporar los criterios de que el menor se encuentra inmerso en actividades o comportamientos para los que no se encuentra preparado ni física ni psicológicamente, sin disponer de la capacidad de consentimiento, transgrediendo la legislación vigente en cada país (Stoltenborgh, Van Ijendoorn, Euser y Bakermans-Kranenbirg, 2011, en Amado, Arce y Herraiz, 2015). En el campo de la investigación social, la mayoría de profesionales hacen uso de los criterios propuestos por Finkelhor y Hotaling (1984), ratificados en España por López (1994). Dichos conceptos han sido el de coerción y la asimetría de edad o diferencias a nivel madurativo, lo que conlleva a una incapacidad a una libre decisión. Dado que el abuso sexual se suele dar en la más estricta intimidad, resulta realmente complicado cuantificar y estimar su prevalencia e incidencia, dada la denominada “cifra negra” de este tipo de situaciones, puesto que parte de los casos no se han denunciado o ni siquiera se han notificado. A pesar de ello, algunos estudios, como el meta-analítico realizado por Pereda, Guilera, Forns y Gómez-Benito (2009), han notificado una prevalencia de entre 7,4% en el caso de los niños y del 19,2% en las niñas...

A.A. Milne - When We Were Very Young : cycle éclectique de chansons pour enfants, chanté par des enfants

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1998 University of Michigan Football Team

1999 University of Michigan Football Team

Bust of a Laughing Young Man

Rembrandt van Rijn, circle of; 1 ft. 4 7/32 in.x 1 ft. 1 5/16 in.; oil on panel