Bollywood directors are now queuing up for the rights of certified hits in Telugu, some of them 10-15 years old.

Online Resource

Online Resource

London : George Bell and Sons, York Street, Covent Garden, 1882-1888.

Tips for healthy joints

No one expected a CRR cut at this time; 75 basis points cut in the policy rate at one shot has also been more than what most had expected

Lewis Library - ML285.5.C6 2019

Lewis Library - ML410.B773 A5 2019

Lewis Library - ML3820.H5613 2019

Lewis Library - ML3917.P58 B65 2019

Lewis Library - ML172.L8713 2019

Lewis Library - ML410.S283 A4 2018

Title: Credit and trade in Later Medieval England, 1353-1532 [electronic resource] / Richard Goddard.
Author: Goddard, Richard, 1967- author.
Imprint: London, [England] : Palgrave Macmillan, [2016]";"©2016
Shelfmark: Ebook Central
Subjects: Business enterprises -- Great Britain -- Finance.
Corporations -- Great Britain -- Finance.

Dewey Library - HG5732.R315 2019

Dewey Library - HG3701.S7313 2019

Late surge glacial conditions on Bakaninbreen, Svalbard, and implications for surge termination Smith, A. M.; Murray, Tavi; Davison, B. M.; Clough, A. F.; Woodward, J.; Jiskoot, Hester Bakaninbreen is a polythermal glacier in southern Spitsbergen, Svalbard, that last surged between 1985 and 1995. Seismic reflection data were acquired during early quiescence in spring 1998, just upstream of the surge front. The results were combined with complementary ground-penetrating radar data to investigate the glacial structure and basal conditions. We find no difference between the ice thickness values determined from the seismic and radar methods, suggesting that any layer of basal ice cannot be greater than 5 m thick. Interpretation of the amplitude of the seismic reflections indicates the presence of permafrost close to the glacier base. A thin layer of thawed deforming sediment separates the glacier from this underlying permafrost. In an area just upstream of the surge front the permafrost becomes discontinuous and may even be absent, the ice being underlain by 10–15 m of thawed sediments overlying deeper bedrock. Highpressure water is believed to have been required to maintain the propagation of the surge, and this area of thawed sediment is interpreted as a route for that water to escape from the basal system. When the surge front passed over this thawed bed, the escaping water reduced the pressure in the subglacial hydraulic system, initiating the termination of the surge. Surge termination was therefore primarily controlled by the presurge permafrost distribution beneath the glacier, rather than any feature of the surge itself. This termination mechanism is probably limited to surges in polythermal glaciers, but the techniques used may have wider glaciological applications. Sherpa Romeo green journal. Permission to archive final published version

Multiple tropical Andean glaciations during a period of late Pliocene warmth Roberts, Nicholas J.; Barendregt, René W.; Clague, John J. The extent and behaviour of glaciers during the mid-Piacenzian warm period illustrate the sensitivity of the cryosphere to atmospheric CO2 concentrations above pre-industrial levels. Knowledge of glaciation during this period is restricted to globally or regionally averaged records from marine sediments and to sparse terrestrial glacial deposits in mid-to-high latitudes. Here we expand the Pliocene glacial record to the tropics by reporting recurrent large-scale glaciation in the Bolivian Andes based on stratigraphic and paleomagnetic analysis of a 95-m sequence of glacial sediments underlying the 2.74-Ma Chijini Tuff. Paleosols and polarity reversals separate eight glacial diamictons, which we link to cold periods in the benthic oxygen isotope record. The glaciations appear to coincide with the earliest glacial activity at high northern latitudes and with events in Antarctica, including the strong M2 cold peak and terminal Pliocene climate deterioration. This concordance suggests inter-hemispheric climate linkages during the late Pliocene and requires that the Central Andes were at least as high in the late Pliocene as today. Our record fills a critical gap in knowledge of Earth systems during the globally warm mid-Piacenzian and suggests a possible driver of faunal migration preceding the large-scale biotic interchange in the Americas during the earliest Pleistocene. Sherpa Romeo green journal. Open access article. Creative Commons Attribution 4.0 International License (CC by 4.0) applies

Cambridge, Massachusetts : The MIT Press, [2019]

An inhibitor of starch-digesting enzymes stunts the growth of certain gut bacteria

An inhibitor of starch-digesting enzymes stunts the growth of certain gut bacteria

Metal may play sleep role through an enzyme responsible for synthesis of norepinephrine