The in Vitro Effect of Metyrapone on Steroid Synthesis in Mice Adrenals at Different Circadian Stages

The circadian rhythm of the in vitro biosynthesis of Cortisol and cortisone in mice adrenals has been documented in the absence and presence of 0.1 μmol metyrapone, an inhibitor of steroid 11β-monooxygenase. After 3 weeks of synchronization with 12 h light: 12 h darkness, adrenalectomy was performed at eight circadian stages: 0, 4, 9, 10, 13, 16, 21, and 22 h after light onset (HALO). Because it has been shown that mice adrenals could convert exogenous 11 -deoxy-cortisol, the synthesis of 11-oxysteroids (Cortisol + cortisone) in adrenal homoge-nates was studied from tritiated precursor. The pattern of steroid synthesis showed a maximum around the end (10 HALO) and a minimum at the beginning of the resting period (0 HALO); the variation was ∼ 10%. A similar pattern was observed in the presence of a ∼50% inhibiting dose of metyrapone. On the other hand, the percent inhibition of 11-oxysteroids synthesis was greater at the beginning of the resting period (0 HALO) and minimum around the end of the activity span (21 HALO), with an overall variation of 20%. However, the variations were statistically insignificant (unpaired t test).     

New data on molluscs and their shell microstructures from the Middle Cambrian Gowers Formation, Australia

Abstract: Numerous new cases of preserved shell microstructure were discovered in molluscs from the Middle Cambrian Gowers Formation (Ptychagnostus atavus/Peronopsis opimus Zone, Floran Stage) in the Georgina Basin, Australia. The new data provide further evidence that, by the Middle Cambrian, molluscan shell microstructures were diverse, and many molluscs had a complex shell with multiple types of shell microstructure. In addition, many new occurrences of laminar microstructures are described herein. For many, the nature of these laminar microstructures is not known, but in three species the microstructure is foliated calcite, and in at least two the microstructure is more likely to have been calcitic semi‐nacre, a type of microstructure known in brachiopods and bryozoans but unknown in modern molluscs. This commonality among these three closely related lophotrochozoans underscores a similar mechanism of biomineralization. Moreover, these observations suggest a prevalence of calcite‐shelled lineages among molluscs from the Middle Cambrian, a time of calcite seas. In addition, the broad occurrence of laminar, nacre‐like microstructures in many of these fossils reveals how widespread these strong (fracture‐resistant) microstructures were in Middle Cambrian molluscs. Additionally, a few specimens of Yochelcionella preserve imprints of a bilaterally symmetrical pair of muscle scars. New taxa described here include Corystos thorntoniensis gen. et sp. nov., Yochelcionella snorkorum sp. nov., Yochelcionella saginata sp. nov., and Anhuiconus? agrenon sp. nov.