A taphonomic approach to the genetic interpretation of clypeasteroid accumulations from the Miocene of Tarragona,NE Spain

Belaústegui, Z., Nebelsick, J.H., Gibert, J.M. de, Domènech, R. & Martinell, J. 2012: A taphonomic approach to the genetic interpretation of clypeasteroid accumulations from the Miocene of Tarragona, NE Spain. Lethaia, Vol. 45, pp. 548–565. Clypeasteroid accumulations are common in Cenozoic shallow marine sediments, particularly in the Neogene, as they are also in analogue modern environments. In this article, four clypeasteroid accumulations from Miocene (Serravallian) shallow marine carbonates of the El Camp de Tarragona Basin (NE Spain) are studied. Two of them are dominated by flat‐shaped Parascutella, whereas the other two consist exclusively of bell‐shaped Clypeaster. The combination of the taphonomic analysis of the tests, the palaeoecological and taphonomic information provided by the associated fossils, and the stratigraphical and sedimentological context of each one of these beds allows interpreting them as autochthonous/parautochthonous accumulations resulting from in situ reworking in moderate energy settings, except for one that constitutes a true sand dollar coquina deposited by a storm event. This contribution explores the potential of thorough taphonomic analysis of marine invertebrate skeletal concentrations and substantiates the importance of clypeasteroid echinoids as producers of shell beds in the Neogene. □ Clypeasteroids, Echinoids, Miocene, Taphonomy, Tarragona.     

Microsatellite loci for the stingless bee Melipona rufiventris (Hymenoptera: Apidae)

Eight microsatellite primers were developed from ISSR (intersimple sequence repeats) markers for the stingless bee Melipona rufiventris. These primers were tested in 20 M. rufiventris workers, representing a single population from Minas Gerais state. The number of alleles per locus ranged from 2 to 5 (mean = 2.63) and the observed and expected heterozygosity values ranged from 0.00 to 0.44 (mean = 0.20) and from 0.05 to 0.68 (mean = 0.31), respectively. Several loci were also polymorphic in M. quadrifasciata, M. bicolor, M. mandacaia and Partamona helleri and should prove useful in population studies of other stingless bees.     

Purine Metabolism in Trypanosomatids*

SYNOPSIS. Purine nucleotide biosynthesis was studied in culture forms of Trypanosoma cruzi strain Y, Crithidia deanei (a reduviid trypanosomatid with an endosymbiote) and an aposymbiotic strain of C. deanei (obtained by curing C. deanei with chloramphenicol). Trypanosoma cruzi was found to synthesize purine nucleotides only from the preformed bases adenine and guanine (“salvage” pathway), adenine being incorporated into both adenine and guanine nucleotides. Similar results were obtained with guanine, indicating that this flagellate has a system for the interconversion of purine nucleotides. Crithidia deanei was able to synthesize purine and pyrimidine nucleotides from glycine (“de novo” pathway) and purine nucleotides from adenine and guanine (“salvage” pathway). Adenine was incorporated into both adenine and guanine nucleotides, while guanine was incorporated into guanine nucleotides only, indicating the presence of a metabolic block at the level of GMP reducaase. The aposymbiotic C. deanei strain was unable to utilize glycine for the synthesis of purine nucleotides, although glycine was utilized for synthesizing pyrimidine nucleotides. These results suggest that the endosymbiote is implicated in the de novo purine nucleotide pathway of the C. deanei-endosymbiote complex. The incorporation of adenine and guanine by aposymbiotic C. deanei strain followed a pattern similar to that observed for C. deanei.     

Cytochrome c-553 is not required for photosynthetic activity in the cyanobacterium Synechococcus.

In cyanobacteria, the water-soluble cytochrome c-553 functions as a mobile carrier of electrons between the membrane-bound cytochrome b6-f complex and P-700 reaction centers of Photosystem I. The structural gene for cytochrome c-553 (designated cytA) of the cyanobacterium Synechococcus sp. PCC 7942 was cloned, and the deduced amino acid sequence was shown to be similar to known cyanobacterial cytochrome c-553 proteins. A deletion mutant was constructed that had no detectable cytochrome c-553 based on spectral analyses and tetramethylbenzidine-hydrogen peroxide staining of proteins resolved by polyacrylamide gel electrophoresis. The mutant strain was not impaired in overall photosynthetic activity. However, this mutant exhibited a decreased efficiency of cytochrome f oxidation. These results indicate that cytochrome c-553 is not an absolute requirement for reducing Photosystem I reaction centers in Synechococcus sp. PCC 7942.     

Isolation and Partial Characterization of a Glycoprotein Complex with Sperm-Receptor Activity from Ciona intestinalis Ovary1

Sperm-egg interaction in the ascidian Ciana intestinalis is mediated by a fucosyl-glycoprotein (FP) component of the egg vitelline coat. FP are responsible for sperm binding, sperm activation and the acrosome reaction. In this paper we report a detailed biochemical and functional characterization of FP purified from the ovaries by affinity chromatography. thic component with sperm receptor activity is a high molecular weight glycoprotein complex (>10⁷) with a protein-carbohydrate ratio of 2:1, which inhibits the binding of the spermatozoa to the vitelline coat and induces sperm activation and the acrosome reaction. Exhaustive proteolytic digestion of FP yields high molecular weight glycopeptides (> 4×10⁵), which contain N-acetylgalactosamine, fucose, galactose and rhamnose. These glycopeptides retain some receptor activity, thus raising the question of the involvement of the polypeptide backbone in the sperm-egg binding process. However, the glycopeptide fraction fails to induce the acrosome reaction: we suggest that the polypeptide fraction plays a role in the induction of sperm activation and the acrosome reaction.     

Acid-base regulation during nitrate assimilation in Hydrodictyon africanum

Abstract The acid-base balance during NO₃^? assimilation in Hydrodictyon africanum has been investigated during growth from (1) an analysis of the elemental composition of the cells, (2) the alkalinity of the ash and (3) the net H⁺ changes in the medium during growth. These investigations agree in showing that some 0.25 excess organic negative charges are generated per N assimilation from No₃^? as N-source and C02 as C-source; the excess OH^? (0.75 OH^? per NO₃^? assimilated) appears in the medium. Approximately half of the excess organic negative charge is attributable to cell wall uronates; the remainder is intracellular. All of the excess OH^? appearing in the medium must have crossed the plasmalemma (as net downhill H⁺ influx or OH^? efflux). Previous work has shown that the value of ψco is more negative than ψ_K⁺ during NO₃^? assimilation, suggesting that the active electrogenic H⁺ extrusion pump is still operative despite the net downhill H⁺ influx. The interpretation of this in terms of H⁺?NO₃^? symport which causes the entry of more H⁺ than is consumed in NO₃^? metabolism, with extrusion of the excess H⁺via the active, electrogenic H⁺ pump, was tested by measuring short-term H⁺ influx upon addition of NO^?₃. A net H⁺ influx occurs before NOa assimilation (as indicated by additional O₂ evolution in the light) has commenced, suggesting a mechanistic relation of H⁺ and NO₃^? influxes. This is consistent with the interpretation suggested above. Determinations of cytoplasmic pH showed no significant effect of NO₃^? assimilation, suggesting that cytoplasmic pH changes sufficient to change the ‘pH-regulating’ H⁺ fluxes are smaller than the errors in the determination of cytoplasmic pH.     

Ca-Cd interaction in the prymnesiophyte Cricosphaera elongata

Abstract. ⁴⁵Ca and ¹⁰⁹Cd uptake were followed in Criscosphaera elongata Prymnesiophyceae. In both cases, after a rapid increase for the first 5 min, the incorporation rate slowed during the hour of observation. Verapamil, a blocker of voltage-dependent slow calcium channels, inhibited ⁴⁵Ca uptake except during the first rapid phase when adsorption should predominate. Cadmium also decreased ⁴⁵Ca labelling, suggesting that the two metals are antagonistic. However, verapamil was shown to augment ¹⁰⁹Cd incorporation, contrary to what occurs in animals cells; this effect is detectable in continuous labelling as well as in pulse experiments. The data support the presence of calcium channels in the alga and suggest several processes in Cd accumulation: adsorption on peripheral envelopes and diffusion of uncharged Cd.     

The Eocene Arctic Azolla bloom: environmental conditions, productivity and carbon drawdown

Enormous quantities of the free-floating freshwater fern Azolla grew and reproduced in situ in the Arctic Ocean during the middle Eocene, as was demonstrated by microscopic analysis of microlaminated sediments recovered from the Lomonosov Ridge during Integrated Ocean Drilling Program (IODP) Expedition 302. The timing of the Azolla phase (~48.5 Ma) coincides with the earliest signs of onset of the transition from a greenhouse towards the modern icehouse Earth. The sustained growth of Azolla , currently ranking among the fastest growing plants on Earth, in a major anoxic oceanic basin may have contributed to decreasing atmospheric p CO₂ levels via burial of Azolla -derived organic matter. The consequences of these enormous Azolla blooms for regional and global nutrient and carbon cycles are still largely unknown. Cultivation experiments have been set up to investigate the influence of elevated p CO₂ on Azolla growth, showing a marked increase in Azolla productivity under elevated (760 and 1910 ppm) p CO₂ conditions. The combined results of organic carbon, sulphur, nitrogen content and ¹⁵N and ¹³C measurements of sediments from the Azolla interval illustrate the potential contribution of nitrogen fixation in a euxinic stratified Eocene Arctic. Flux calculations were used to quantitatively reconstruct the potential storage of carbon (0.9–3.5 10¹⁸ gC) in the Arctic during the Azolla interval. It is estimated that storing 0.9 10¹⁸ to 3.5 10¹⁸ g carbon would result in a 55 to 470 ppm drawdown of p CO₂ under Eocene conditions, indicating that the Arctic Azolla blooms may have had a significant effect on global atmospheric p CO₂ levels through enhanced burial of organic matter.