Revised age model of DSDP Site 95-612

Alkenone-based Cenozoic records of the partial pressure of atmospheric carbon dioxide (pCO2) are founded on the carbon isotope fractionation that occurred during marine photosynthesis (epsilon [p37:2]). However, the magnitude of epsilon [p37:2] is also influenced by phytoplankton cell size - a consideration lacking in previous alkenone-based CO2 estimates. In this study, we reconstruct cell size trends in ancient alkenone-producing coccolithophores (the reticulofenestrids) to test the influence that cell size variability played in determining epsilon [p37:2] trends and pCO2 estimates during the middle Eocene to early Miocene. At the investigated deep-sea sites, the reticulofenestrids experienced high diversity and largest mean cell sizes during the late Eocene, followed by a long-term decrease in maximum cell size since the earliest Oligocene. Decreasing haptophyte cell sizes do not account for the long-term increase in the stable carbon isotopic composition of alkenones and associated decrease in epsilon [p37:2] values during the Paleogene, supporting the conclusion that the secular pattern of epsilon [p37:2] values is primarily controlled by decreasing CO2 concentration since the earliest Oligocene. Further, given the physiology of modern alkenone producers, and considering the timings of coccolithophorid cell size change, extinctions, and changes in reconstructed pCO2 and temperature, we speculate that the selection of smaller reticulofenestrid cells during the Oligocene primarily reflects an adaptive response to increased [CO2(aq)] limitation.

(Table T1) Paleomagnetic properties of ODP Hole 191-1179D basalts

During Ocean Drilling Program Leg 191, ~100 m of mid-Cretaceous igneous crust was cored at Site 1179 (41.08°N, 159.96°E), located within magnetic Anomaly M8 on the abyssal plain of the northwest Pacific Ocean near Shatsky Rise. Paleomagnetic data from this section are significant because they can constrain the mid-Cretaceous Pacific plate paleolatitude and paleomagnetic pole, both of which can be used to infer tectonic drift and other geodynamic processes. In this study, we analyzed the paleomagnetism of 122 samples from 40 flows in the Site 1179 basalt section. Comparison of inclination data among flows implies 13 independent measurements of the paleomagnetic field. Assuming a reversed magnetic polarity because of the site location within Anomaly M8, the data give a mean paleocolatitude of 88.1° ± 6.8° (corresponding to a paleolatitude of 1.9°N). The paleocolatitude is consistent with other mid-Cretaceous Pacific paleomagnetic data that indicate ~39° northward drift of the western Pacific plate since mid-Cretaceous time. Comparison of observed between-flow colatitude variance with that expected from secular variation data suggests that secular variation may not have been completely averaged with the 13 independent groups sampled at Site 1179. Colatitude scatter in the section is markedly less in the deepest 33 m of the hole, indicating a shift from rapidly erupted flows in the bottom ~33 m of the section to more slowly emplaced flows above.

Estimates of %NCW bathing deep North Atlantic (IODP Site 306-U1313) over the past ~3.3 Ma

The circulation and internal structure of the oceans exert a strong influence on Earth's climate because they control latitudinal heat transport and the segregation of carbon between the atmosphere and the abyss (Sigman et al., 2010, doi:10.1038/nature09149). Circulation change, particularly in the Atlantic Ocean, is widely suggested (Bartoli et al., 2005, doi:10.1016/j.epsl.2005.06.020; Haug and Tiedemann, 1998, doi:10.1038/31447; Woodard et al., 2014, doi:10.1126/science.1255586; McKay et al., 2012, doi:10.1073/pnas.1112248109) to have been instrumental in the intensification of Northern Hemisphere glaciation when large ice sheets first developed on North America and Eurasia during the late Pliocene, approximately 2.7 million years ago (Bailey et al., 2013, doi:10.1016/j.quascirev.2013.06.004). Yet the mechanistic link and cause/effect relationship between ocean circulation and glaciation are debated. Here we present new records of North Atlantic Ocean structure using the carbon and neodymium isotopic composition of marine sediments recording deep water for both the Last Glacial to Holocene (35-5 thousand years ago) and the late Pliocene to earliest Pleistocene (3.3-2.4 million years ago). Our data show no secular change. Instead we document major southern-sourced water incursions into the deep North Atlantic during prominent glacials from 2.7 million years ago. Our results suggest that Atlantic circulation acts as a positive feedback rather than as an underlying cause of late Pliocene Northern Hemisphere glaciation. We propose that, once surface Southern Ocean stratification (Sigman, et al., 2004, doi:10.1038/nature02357) and/or extensive sea-ice cover (McKay et al., 2012, doi:10.1073/pnas.1112248109) was established, cold-stage expansions of southern-sourced water such as those documented here enhanced carbon dioxide storage in the deep ocean, helping to increase the amplitude of glacial cycles.

Heiligenspielrezeption in der Schweiz 1929: Das Bruderklausenspiel von Oskar Eberle

Based on Hansjürgen Linke’s study about the history of the reception of religious and secular medieval plays in twentieth-century Germany, the paper examines the respective situation in Switzerland. It focusses on the Bruderklausenspiel (1929), written and staged by Oskar Eberle. The director and scholar Oskar Eberle, and the Schweizerische Gesellschaft für Theaterkultur (SGTK) were the most influential supporters of the reception of religious plays in twentieth-century Switzerland. While in Germany the revival of medieval theatre emphasized a Renaissance of a former national importance, in Switzerland, the situation was very different. The revival of religious plays had a certain confessional background, and the political idea was to strengthen national self-confidence, and to confirm the nation’s historical neutrality concerning foreign affairs.

Cori celebri per voci d'uomini.

Cover title.

Hail, Ceres, hail : cantata for soprano and alto soli, and chorus of mixed voices /

For soloists (SA), chorus (SATB), and piano.

The broken troth : a legend of old Fort Union : a cantata for soprano and tenor solo with chorus, four-part, for women's voices /

"Op. 32."

Arion : a collection of four-part songs for male voices, in separate vocal parts with piano score, mainly to be sung without accompaniment /

Mode of access: Internet.

Montfort : eine Rheinsage von F. v. Hoffnaass : für Soli, Chor und Orchester = A legend of the Rhine : composed for soli, chorus & orchestra: op. 145 /

Mode of access: Internet.

Parsifal

Mode of access: Internet.

Die Mai-Königin, Pastorale.

Mode of access: Internet.

Kreuzfahrer. Op. 50 (S.- T.- Bass-Solo u. gem. Chor)

Original Danish words by C. C. T. Andersen, with German translation.

Jakob van Artevelde : Feestkantate /

"La 1re exécution de cette oeuvre a eu lieu ... à Gand, le 14 septembre 1863, jour de l'inauguration de la statue de Jacques van Artevelde."

The bride, a cantata

Mode of access: Internet.

Roméo et Juliette; : symphonie dramatique avec choeurs, solos de chant et prologue en récitatif choral, composée d'après la tragedie de Shakespeare. Op. 17. /

Symphony, with vocal solos and chorus; French and German words.