İzmir‐Ankara suture as a Triassic to Cretaceous plate boundary – data from central Anatolia

The İzmir‐Ankara suture represents part of the boundary between Laurasia and Gondwana along which a wide Tethyan ocean was subducted. In northwest Turkey, it is associated with distinct oceanic subduction‐accretion complexes of Late Triassic, Jurassic and Late Cretaceous ages. The Late Triassic and Jurassic accretion complexes consist predominantly of basalt with lesser amounts of shale, limestone, chert, Permian (274 Ma zircon U‐Pb age) metagabbro and serpentinite, which have undergone greenschist facies metamorphism. Ar‐Ar muscovite ages from the phyllites range from 210 Ma down to 145 Ma with a broad southward younging. The Late Cretaceous subduction‐accretion complex, the ophiolitic mélange, consists of basalt, radiolarian chert, shale and minor amounts of recrystallized limestone, serpentinite and greywacke, showing various degrees of blueschist facies metamorphism and penetrative deformation. Ar‐Ar phengite ages from two blueschist metabasites are ca. 80 Ma (Campanian). The ophiolitic mélange includes large Jurassic peridotite‐gabbro bodies with plagiogranites with ca. 180 Ma U‐Pb zircon ages. Geochronological and geological data show that Permian to Cretaceous oceanic lithosphere was subducted north under the Pontides from the Late Triassic to the Late Cretaceous. This period was characterized generally by subduction‐accretion, except in the Early Cretaceous, when subduction‐erosion took place. In the Sakarya segment all the subduction accretion complexes, as well as the adjacent continental sequences, are unconformably overlain by Lower Eocene red beds. This, along with the stratigraphy of the Sakarya Zone indicate that the hard collision between the Sakarya Zone and the Anatolide‐Tauride Block took place in Paleocene

NCSS Notable Trade Book Lesson Plan <i>Everybody Works</i> by Shelley Rotner &amp; Ken Kreisler

Everybody Works in many ways, indoors, outdoors, at home, at an office, by traveling from place to place, to earn income, or as a hobby. This book is a photographic essay looking at the many ways in which people work and sometimes use animals in work. The learning cycle lesson helps young children construct a deeper understanding of work as varied and an important part of each person’s life.</jats:p

What Does Peace Mean? Kindergarteners Share Ideas

Kindergarteners’ (n=41) concept of peace, a foundational social studies concept, was investigated via pre- and post-assessments that first, asked them to physically demonstrate how they looked or felt when they were at peace, second, asked them to draw a scene showing peace, and third, to caption the drawing. In pre-assessments all but three children demonstrated aggression and drew aggressive stances accompanied by captions indicating aggression. After opportunities to read about, discuss, and explore the concept of peace over five weeks, post-assessment occurred. In the post-assessments none of the data indicated aggression. Categories coded showed peace described as enjoyable activities, pro-social behaviors, and quietness/calmness/privacy. The study suggests hypotheses for further research investigating the concept of peace among very young children and possible factors influencing their concept and implications for social studies curriculum.</jats:p

Monoamine oxidase inhibitory activities of novel 3,4-dihydroquinolin-(1H)-2-one derivatives

Three 3,4-dihydroquinoline-(1H)-2-one derivatives were synthesized and their monoamine oxidase (MAO) inhibitory activities were evaluated. The calculated IC50 values revealed that compound Q (N-amino-3,4-dihydroquinoline-(1H)-2-one), which carries a free amine group in the molecule, inhibited rat liver MAO-B competitively and reversibly suggesting that this relatively small compound may interact with the active site channel of the enzyme while the compounds QB (1-(benzlyden-amino)-3,4-dihydroquinoline-(1H)-2-one), PCN (2-(3-cyano-2-oxo-4-phenyl-2H-quinolin-1-yl-N-cyclohexyl-2-(4'-chlorophenyl) acetamide) and MG (tert-butyl-N-[cyclohexylcarbamoyl-(3-hydroxyphenyl)methyl]-N-(2-benzoylphenyl)-carbamate) inhibited rat liver MAO-B non-competitively and irreversibly, suggesting that these compounds may interact with another hydrophobic binding region outside of the active site of the enzyme

Uplift of Anatolia

The Cenozoic history of the Anatolian Plateau is investigated using the distribution of the last Cenozoic marine strata, the ages of Neogene continental sediments and magmatic rocks, and thermochronology. In central and northern Anatolia, the youngest marine sediments are of Middle Eocene age and show that the region has been above the sea level since ca. 41 Ma. The preservation of marine Eocene sequences over large regions and widespread distribution of Neogene continental sediments point to minor erosion or subsidence, except in the Miocene core complexes, and indicate average surface uplift or subsidence rates of less than 0.05 km/Myr since 41 Ma. The Cenozoic mammal ages point to widespread continental deposition on the Anatolian Plateau from Early Miocene (ca. 22 Ma) to the present, and a similar pattern of semicontinuous magmatism has been observed in Anatolia since ca. 23 Ma. New thermochronological data from central Anatolia to west of Ankara have indicate a major exhumation phase during the Paleocene and Early Eocene, followed by minor uplift and/or subsidence. Miocene exhumation is restricted to the core complexes, such as the Kazda\u11f Massif. The Anatolian Plateau has been a land area since 41 Ma and was characterized by continental sedimentation and volcanism in the last 22 Myr. In this period, subsidence and uplift were balanced so that central Anatolia was maintained above sea level. In contrast, its southern mountainous margin, the Taurides, is free of Neogene magmatism and has undergone a fast uplift above sea level since 8 Ma (ca. 0.3 km/Myr). These differences indicate that the uplift of Anatolia cannot be ascribed to a single mechanism. Flat subduction, followed by mantle upwelling under Anatolia in the post-Middle Eocene period, maintained the region above the sea level, whereas the Late Miocene rupture of the subducting eastern Mediterranean oceanic slab have induced fast uplift of the Taurides