The oceanic base of slope record of the Permian-Triassic crisis: view from Tethys (Oman)

The Oman Mountains provide some of the best sections of Permian and Triassic sediments from ocean sea floor to base-of-slope environments related to the distal South Tethyan margin. The central part of the range exposes the Buday'ah section of oceanic sediments in the so-called "Hawasina allochtons". The locality of Wadi Maqam in the north-western part of the Oman Mountains is among places where the thick Permian-Triassic base-of-slope sediments is exposed (Baud et al., 2001). Overlying 400 m of middle Permian limestones and dolomites, the upper Permian sediments consist of 50 m of ≈ 10 cm thick beds of cherts and dolomites rich in sponge spicules. The top of the Permian units is well bioturbated lime mudstone-wackestone, devoid of cherts and dated as late Changhsingian (Krystyn in Richoz et al., 2005). The boundary yellow shales are overlain by very thinly bedded, laminated microbial platy lime mudstone with H. parvus. The dramatic loss of the burrowing infauna indicates the appearance of oxygen-poor water. These Induan sediments are about 25 m thick and show at the top the first calcirudites, commonly clast-supported (edge-wise conglomerates), and are characterized by tabular clasts representing the sub- in situ reworking of the laminated, platy calcilutite. The very thick Smithian overlying litho-unit (up to 900 m) marks the onset on the base-of-slope of a deep-marine basin in which carbonate submarine fan deposits developed This very thick unit consists essentially of platy limestones, calcarenites and calcirudites. It comprises mainly grey-beige calcilutite, laminated and flaggy, interbedded with sparse beds of fine-grained calcarenite in cm beds. Channelized beds of intraformational calcirudite are also part of this succession which constitutes the greater part of the outcrop available. During the Spathian to Anisian, the sedimentation changes to terrigenous mudstone and siltstone that ended with Ladinian radiolarites.

Adrenal crisis presenting as hypoglycemic coma.

An 18-month-old male infant presented with hypoglycemic coma and clinical signs of bronchopneumonia. He was suspected of suffering from septic shock. The patient progressed to irreversible multiple organ failure before the diagnosis of adrenal crisis was established. Plasma levels of ACTH and cortisol remained undetectable. Renin and aldosterone were normal. An autopsy failed to demonstrate any adrenal gland cortical tissue. Immunohistochemical staining demonstrated the presence of all pituitary hormones except ACTH, establishing the diagnosis of isolated ACTH deficiency. Intensive care clinicians should consider adrenal crisis in non-diabetic children with hypoglycemia and rapid circulatory deterioration.

Interbank liquidity crunch and the firm credit crunch: Evidence from the 2007-2009 crisis

We study the credit supply effects of the unexpected freeze of the Europeaninterbank market, using exhaustive Portuguese loan-level data. We find thatbanks that rely more on interbank borrowing before the crisis decrease theircredit supply more during the crisis. The credit supply reduction is stronger forfirms that are smaller, with weaker banking relationships. Small firms cannotcompensate the credit crunch with other sources of debt. Furthermore, theimpact of illiquidity on the credit crunch is stronger for less solvent banks.Finally, there are no overall positive effects of central bank liquidity, but higherhoarding of liquidity.

Monetary policy in a systemic crisis

This paper examines the monetary policy followed during the current financial crisisfrom the perspective of the theory of the lender of last resort. It is argued that standardmonetary policy measures would have failed because the channels through whichmonetary policy is implemented depend upon the well functioning of the interbankmarket. As the crisis developed, liquidity vanished and the interbank market collapsed,central banks had to inject much more liquidity at low interest rates than predicted bystandard monetary policy models. At the same time, as the interbank market did notallow for the redistribution of liquidity among banks, central banks had to design newchannels for liquidity injection.