Auxin and gibberellin-like substances in coconut milk and malt extract

Auxin-like and gibberellin-like activity was detected in both coconut milk and malt extract. Indole-3-acetic acid was tentatively identified as being present in malt extract. The results obtained correlate well with the responses reported by researchers using coconut milk and malt extract as additives to basal nutrient media in tissue culture experiments.     

Synthesis and analysis of potent, more lipophilic derivatives of the bradykinin B2 receptor antagonist peptide Hoe 140.

Bradykinin (BK) is an endogenous peptide that has been implicated in several pathological conditions, hence antagonists of its activity have therapeutic potential. The decapeptide Hoe 140 is currently one of the best BK antagonists, but interest remains in finding even more potent compounds. A library of Hoe 140 derivatives was synthesized that incorporated non-natural analogs of the cationic, naturally occurring amino acids arginine (Arg) and lysine (Lys). The modified amino acids were designed to form enhanced ionic interactions due to an increase in local hydrophobicity, which promotes desolvation of the cation in water. The potencies of the resulting peptides were determined by competitive binding assays in human A431 cells expressing the BK B2 receptor. Two of the peptides synthesized were equipotent to Hoe 140 (IC(50s) 2.99 and 3.36 nM) and the most potent was demonstrated as a functional antagonist in vitro by blocking BK-mediated phosphorylation of mitogen-activated protein (MAP) kinases. The new derivatives are more hydrophobic than Hoe 140 and thus may exhibit changes in pharmacokinetic properties when evaluated in vivo.     

Magnesian calcite and chamositic ooids forming shoals peripheral to Late Ordovician (Ashgill) muddy siliciclastic shores: southern Ontario

In southern Ontario, ooids are associated with two distinct facies associations in the Queenston Formation, the final stage of Late Ordovician (Ashgill) Taconic basin fill. One facies consists of thin ooid and bioclastic grainstones interbedded with mudrock, and lies near the base of the formation, and, in southwestern Ontario, also forms a local NW-thickening wedge near the middle of the formation. Ooids have radial-fibrous and radial-concentric fabrics (Type A), with chamosite, illite, and Fe-oxide laths at intercrystalline sites. Vertical lithologic and ooid abundance patterns indicate that thresholds to carbonate production were sensitive to changes in terrigenous sediment supply, sea level, circulation, accommodation space, and tectonism.

Ooids in the second facies association are admixed with abraded fragments of open-marine biota, or occur burrow fills, within a <30-cm-thick interval of mudrock near the top of the preserved Queenston succession, a few metres below the Ordovician–Silurian unconformity. Ooids have radial concentric and crosscutting patchy microcrystalline fabrics (Type B). This unit may represent a transgressive or stillstand deposit modified by bioturbation.

The extent of preserved fabric suggests that both ooid types were originally magnesian calcite, but Type A ooids underwent greater burial alteration. This is shown by crystalline mosaics that cross-cut relict primary fabrics; δ¹³C values (−1.82‰ to +0.67‰) and δ¹⁸O values (−4.46‰ to −10.57‰) more negative than marine calcite of similar age; Mn and Fe concentrations more elevated above expected marine values; and a luminescence similar to that of intergranular cements. Burial meteoric diagenesis was likely promoted by excellent permeability of the host sand. We interpret authigenic chamosite and Fe-oxide to reflect diagenesis of iron-bearing and clay detritus trapped during ooid growth. Type B ooids suffered less alteration: δ¹³C (+1.1‰ to +6.64‰) and δ¹⁸O (−3.04‰ to −4.81‰) values overlap the expected marine range, including ¹³C enrichment that occurs within the Hirnantian (latest Ordovician) excursion. Although Mn and Fe values are still higher than those of modern calcitic ooids, negligible luminescence suggests that recrystallization occurred in the presence of marine-derived pore fluids. Further burial alteration was inhibited due to low permeability of the host mud.

Type A ooid facies in the Queenston Formation forms an ancient analogue for lesser known Quaternary ooid shoals peripheral to tropical deltaic systems. The facies of Type B ooids, while more enigmatic, may preserve a geochemical herald of latest Ordovician climate change. The presence of minor chamosite in Type A ooids defines a possible distal facies of the well-known oolitic ironstones of similar age in the mid-continental USA.     

High-performance liquid chromatographic determination of hydrocortisone and methylprednisolone and their hemisuccinate esters in human serum

A high-performance liquid chromatographic method is described for the simultaneous determination of methylprednisolone (MP) and methylprednisolone hemisuccinate (MPHS), or hydrocortisone (HC) and hydrocortisone hemisuccinate (HCHS) in human serum. Reversed-phase liquid chromatography was performed on a microparticulate C₁₈ column (Spherisorb, 5 μm) using a mobile phase of 2% glacial acetic acid, 30–35% acetonitrile, 70–65% water with ultraviolet detection (254 nm). The method uses 17α-hydroxyprogesterone as the internal standard for the determination of methylprednisolone and its hemisuccinate ester, or 11-deoxy-17-hydroxycorticosterone as the internal standard for the determination of hydrocortisone and its hemisuccinate ester. The sensitivity is 0.03 μg/ml for HC, 0.07 μg/ml for MP, 0.04 μg/ml for MPHS, and 0.10 μg/ml for HCHS, with a detection limit of 0.02 μg/ml for all four steroids. Calibration curves are linear up to 3 μg/ml for MP or MPHS (as equivalent MP) and up to 4 μg/ml for HC and 7 μg/ml (as equivalent HC) for HCHS. The pooled relative standard deviation for replicate samples for each steroid is < 7%. Plasma concentration—time curves are reported for MP and MPHS or HC and HCHS of two human subjects following intramuscular administration of 125 mg of methylprednisolone sodium succinate for injection, U.S.P., or 250 mg of hydrocortisone sodium succinate for injection, U.S.P.     

Mechanism of acridine orange interaction with phospholipids and proteins in renal microvillus vesicles

The mechanism of interaction of acridine orange (AO), a fluorescent, weak base, with rabbit kidney brush border membrane vesicles (BBMV) has been studied by absorption, and steady-state and time-resolved fluorescence spectroscopy. Equilibrium binding experiments indicate that AO binds to an apparent single class of sites on BBMV with a dissociation constant of 90 microM and site stoichiometry of 810 nmol/mg protein. The absorption spectra AO indicate that BBMV induces aggregation of AO; experiments with lipid vesicles show that the aggregation requires BBMV membrane proteins. Fluorescence stopped-flow experiments in which 0.15 mg/ml BBMV is mixed with increasing concentrations of AO result in a time course of fluorescence enhancement for [AO] less than 1.5 microM, and of fluorescence quenching for [AO] greater than 1.5 microM. Similar stopped-flow experiments with phosphatidylcholine lipid vesicles result only in a fluorescence enhancement time course. These results indicate the presence of two parallel pathways for AO binding to BBMV: one for AO binding to BBMV lipid, the other for AO binding to BBMV protein. Nanosecond lifetime measurements and fluorescence titration experiments confirm the presence of two environments for AO in BBMV. Fluorescence stopped-flow experiments indicate that AO responds to the imposition of an outwardly directed proton gradient by a rapid (less than 0.5 s) decrease in fluorescence, corresponding to re-equilibration of AO into the acidic intravesicular compartment, followed by an increase in fluorescence, corresponding to proton flux across the membrane. These findings have been incorporated into a stepwise mechanism for AO interaction with BBMV which have direct implications for the use of AO as a pH indicator in biological systems.     

Marine saline ponds as sedimentary archives of late Holocene climate and sea-level variation along a carbonate platform margin: Lee Stocking Island, Bahamas

A 1500-year, late Holocene history of coastal and lacustrine carbonate sedimentation is preserved in shallow ponds on Lee Stocking Island, Exuma Cays, Bahamas. Details of environmental change have been extracted by integrating lithostratigraphy, biostratigraphy (macrobiota, foraminifers, ostracodes), and chemical stratigraphy (C, O isotopes of foraminiferal and molluscan skeletal carbonate; MgO wt% of ostracode calcite) with a well defined ¹⁴C AMS radiocarbon chronology. Carbonate deposition began within physically restricted, euryhaline coastal embayments, with several pronounced changes in salinity defined by biotic and calculated salinity variation (from MgO wt% in shells of Cyprideis americana). By about 700–740 yr B.P., embayment closure occurred possibly related to changed longshore deposition associated with sea level rise and/or regional change in climate (previously documented). With closure, the initial euryhaline foraminifer assemblage was replaced by a predominant hypersaline biofacies (e.g., Triloculina sp.); with progressive basin fill, ostracode assemblages, calculated salinities, and variation in abundance of the gastropod Cerithidea sp. may resolve higher-order (and some extreme) salinity fluctuations throughout the remaining history of saline pond development. Foraminiferal isotope stratigraphy is compatible with that expected for hydrologically closed lake basins. Carbonate accumulation was effectively shut-down <200 years ago, replaced by stromatolitic growth. Present-day salinities vary according to water balance governed by rainfall and evaporation. A centuries-scale (300–400 year) flux of abraded (reworked), marine-derived bioclasts, admixed with skeletal remains of indigenous biota, is also preserved in these ponds. Allochthonous sediment was transported by hurricane storm surges or related to abrupt transgressive events superimposed on an overall gradual rise in global sea level. We discuss evidence for both as controls on sedimentation. Our study illustrates that saline ponds on Bahamian islands are excellent sedimentary archives of local, regional, and possibly global paleoclimatic events of late Holocene age.