Spatial variation in selection in a plant-pollinator system in the wadis of Sinai,Egypt

We studied an insect-plant pollination system in adjacent steep-sided wadis and a connecting plain in the mountains of southern Sinai (Egypt): this environment creates a strongly divided habitat, which may promote the local differentiation of sub-populations. We tested for spatial differences in phenotypic reproductive characters of the only plant flowering abundantly in early spring, Alkanna orientalis (Boraginaceae), and its major pollinator at that time of year, Anthophora pauperata (Apoidea, Anthophoridae). There were significant morphological differences between sub-populations of Alkanna, mainly between plants from the narrower wadis and those on the interconnecting plain. Flowers on the plain were larger, with wider corollas and more nectar standing crop; these plants retained more flowers on the inflorescence, but received many fewer visits to flowers. There was a significant selection gradient between flower size and maternal fitness (seed set) in the plain, but not elsewhere. Natural selection may have increased resources devoted to attracting insect visitors in response to fewer pollinating visits in the plain. Consistent with this explanation, by experimentally manipulating flower number per plant, we showed that within a wadi having more flowers on a plant secured more visits.     

87Sr/86Sr Chronostratigraphy and dolomitization history of the Seroe Domi Formation,Curaçao (Netherlands Antilles)

Summary The Seroe Domi Formation is a 350 m-thick sequence of Neogene marine limestones and silicilastic sandstones cropping out on the leeward coast of Cura?ao, Netherlands Antilles. Integrated analyses of lithofacies, biostratigraphy, geochemistry and Sr isotope model age analyses indicate that Seroe Domi Formation has experienced three major episodes of limestone diagenesis and dolomitization (Dolomites I, I′, and II) that have taken place after successive Mio-Plio-Pleistocene depositional and subaerial exposure events (Subunits 1, 2, and 3). Subunit 1, the lowermost 30 to 100 m of the Seroe Domi Formation, is composed of interbedded coralgal grainstone gravity flows, pelagic wackestones, and allochthonous blocks deposited in Middle Miocene deep-water (>500 m) fore-reef and carbonate slope environments. Subunit 2, the uppermost 250 m of the Seroe Domi Formation, consists of coralgal packstones with basement-derived siliciclastic sands that were deposted in shallowing fore-reef to reef-front environments during the Late Miocene to Pliocene. Subunit 3 siliciclastic sandstones were deposited during the Early Pleistocene within erosional cavities in the Subunit 2 limestones, and are overlain by Late Pleistocene Quaternary Limestone Terraces. The petrography, distribution and geochemistry of Dolomites I, I′ and II indicate that they were precipitated from seawater-freshwater mixing zone fluid environments. Dolomite rhombs and meteoric calcite cements within biomolds illustrate that the host Seroe Domi Formation limestones were subaerially exposed prior to each dolomitization event. Dolomite I (δ¹⁸O = +1.04 to +2.46% PDB; δ¹³C = −2.55 to −6.79 PDB;⁸⁷Sr/⁸⁶Sr=0.708866 to 0.708915; Zn=0 ppm; Cu=0 ppm) was precipitated from mixtures of seawater with isotopically-depleted freshwater during the late Middle Miocene. Dolomite I′ (δ¹⁸O = +2.08 to +3.55 PDB, δ¹³C = −1.53 to 1.69 PDB,⁸⁷Sr/⁸⁶Sr=0.708981−0.709030; Zn=0 ppm; Cu=0 ppm) was also precipitated from mixtures of seawater with isotopically-depleted freshwater, but during late Late Miocene. In contrast, Dolomite II (δ¹⁸O = +2.69 to +3.51 PDB; δ¹³C = −0.34 to +1.53 PDB;⁸⁷Sr/⁸⁶Sr=0.708954 to 0.709088; Zn=20 ppm; Cu=20 ppm) precipitated from late Early Pliocene mixtures of seawater with isotopically-depleted freshwater that had derived Zn, Cu, and less-radiogenic Sr from basalts comprising the Cura?ao basement.     

Cyclone-induced Shift in Foraging Behavior in Flying Foxes in American Samoa1

Tropical cyclones pass over or near American Samoa on average about once every 3 years. Because many trees may be stripped of leaves, flowers, and fruit, cyclones exert a major impact on the feeding ecology of nectivorous and frugivorous flying foxes. We examined search time and in-tree time immediately postcyclone (3–6 weeks) and during a recovery period (15–16 months after the last cyclone). Both Pteropus tonganus and P. samoensis increased search time and decreased tree time (an indication of less food available per tree) immediately after the passage of cyclone Ofa.     

Multiplex single molecule counting technology used to generate interleukin 4, interleukin 6, and interleukin 10 reference limits

Detecting biomarkers at pg/ml concentrations or below is, in many situations, critical for quantifying levels in healthy individuals as well as the changes that can occur in the progression of disease states. The ability to detect multiple biomarkers from the same sample allows for better diagnoses, more efficient testing, and lower volumes of sample required. Based on single molecule counting technology, a multiplex instrument was designed and built that is capable of detecting cytokines and other low-abundance proteins at sub-pg/ml quantities in human plasma samples. The multiplex single molecule counting instrument was used to generate 95% reference limits for interleukin 4 (IL-4, <0.61 pg/ml), interleukin 6 (IL-6, <6.53 pg/ml), and interleukin 10 (IL-10, <1.08 pg/ml) from 100 healthy human donor plasma samples, with more than 90% of IL-4 concentrations and 100% of IL-6 and IL-10 concentrations above the limit of detection.     

Calcium current in embryonic Xenopus muscle cells in culture

We have investigated the appearance of calcium current in Xenopus muscle cells in 1- to 6-day-old cultures. Whole cell currents were recorded using a patch-clamp amplifier with sodium and potassium replaced with tetraethylammonium and cesium, respectively, and BaCl2 used in place of CaCl2. When the muscle membrane was depolarized above -30 mV, a slow inward current was activated, the current reached a peak amplitude near 0 mV, and an outward current became apparent above +10 mV. This slow current was enhanced by adding barium or Bay K 8644 to the extracellular recording solution and was blocked by the addition of cobalt, cadmium, or the dihydropyridines nifedipine or (+)PN 200-110. Taken together these results indicate the presence of an inward calcium current mediated through L-type channels. Thirty-one percent of the cells examined on the first day in culture showed no discernible slow inward current; however, as the age of the culture increased, all cells showed slow inward current and there was an increase in the amplitude of the current. A small proportion of the muscle cells (5 out of 34) also showed a fast activating and inactivating inward current. This current, which activated at more hyperpolarized potentials (-40 mV) was only present when 5 mM ATP was included in the internal recording solution. It also appeared to be mediated through a calcium channel but not a dihydropyridine, sensitive channel.     

Surface hydrophobicity and dispersal of Pseudomonas aeruginosa from biofilms

A novel method of cell culture was employed to control the growth-rate of bacterial biofilms [1]. Cell-surface hydrophobicity increased progressively with growth rate for planktonic, chemostatgrown Pseudomonas aeruginosa and also for cells, resuspended from the biofilms. Dependence of surface hydrophobicity upon growth rate was greater for the planktonic cells. Newly-formed daughter cells, shed from the biofilms, were in all cases more hydrophilic than their adherent counterparts and demonstrated only slight growth rate dependency for this property.