{[N.N.], Szenenfoto, Gruppenbildnis, in: William Shakespeare: Was ihr wollt, Theater Basel

Signatur des Originals: S 36/F12219

Ritter Nicolo Paganini der erste Violinspieler seiner Zeit auf den National-Theater in Nürnberg den 9. Nov. 1829.

Signatur des Originals: S 36/G01835

Wolfgang Amadeus Mozart {[u.a.], Gruppenbildnis, im Theater

Signatur des Originals: S 36/G01712

Theater zu Tien-Sin.

Signatur des Originals: S 36/G02686

Désirée Artôt de Padilla als Rosina, Rollenbild, in: Gioacchino Rossini, Il barbiere di Siviglia, Berlin: Victoria Theater

Signatur des Originals: S 36/G12721

Désirée Artôt de Padilla als Rosina, Rollenbild, in: Gioacchino Rossini, Il barbiere di Siviglia, Berlin: Victoria Theater

Signatur des Originals: S 36/G12722

Enrico delle Sedie als Figaro, Rollenbild, in: Wolfgang Amadeus Mozart: Il barbiere di Siviglia, Berlin: Victoria-Theater

Signatur des Originals: S 36/G12946

Das Theater.

Signatur des Originals: S 36/G13856

Das Theater zu Wiesbaden

Signatur des Originals: S 36/G03873

Das Theater in Wiesbaden.

Signatur des Originals: S 36/G13874

Thalia Theater, Frankfurt a. M., Innenansicht

Signatur des Originals: S 36/G14532

Thalia Theater, Frankfurt a. M., Innenansicht

Signatur des Originals: S 36/G14533

Braunschweiger Moden-Courier [Elektronische Ressource]] : Zeitschrift für Literatur, Kunst, Theater und Mode

Online-Ressource

Stable isotopes and element concentrations of samples from the Wadi Bih, United Arab Emirates

Ocean acidification triggered by Siberian Trap volcanism was a possible kill mechanism for the Permo-Triassic Boundary mass extinction, but direct evidence for an acidification event is lacking. We present a high-resolution seawater pH record across this interval, using boron isotope data combined with a quantitative modeling approach. In the latest Permian, increased ocean alkalinity primed the Earth system with a low level of atmospheric CO2 and a high ocean buffering capacity. The first phase of extinction was coincident with a slow injection of carbon into the atmosphere, and ocean pH remained stable. During the second extinction pulse, however, a rapid and large injection of carbon caused an abrupt acidification event that drove the preferential loss of heavily calcified marine biota.