Evolutionary diversification of reef corals: a comparison of the molecular and fossil records

Understanding historical patterns of diversity dynamics is of paramount importance for many evolutionary questions. The fossil record has long been the only source of information on patterns of diversification, but the molecular record, derived from time-calibrated phylogenies, is becoming an important additional resource. Both fossil and molecular approaches have shortcomings and biases. These have been well studied for fossil data but much less so for molecular data and empirical comparisons between approaches are lacking. Here, we compare the patterns of diversification derived from fossil and molecular data in scleractinian reef coral species. We also assess the robustness of molecular diversification rates to poor taxon sampling. We find that the temporal pattern of molecular diversification rates is robust to incomplete sampling when rates are calculated per interval. The major obstacle of molecular methods is that rate estimates are distorted because diversification rates can never be negative, whereas the fossil record suffers from incomplete preservation and inconsistent taxonomy. Nevertheless, the molecular pattern of diversification is comparable to the pattern we observe in the fossil record, with the timing of major diversification pulses coinciding in each dataset. For example, both agree that the end-Triassic coral extinction was a catastrophic bottleneck in scleractinian evolution.     

Marine extinction risk shaped by trait–environment interactions over 500 million years

Perhaps the most pressing issue in predicting biotic responses to present and future global change is understanding how environmental factors shape the relationship between ecological traits and extinction risk. The fossil record provides millions of years of insight into how extinction selectivity (i.e., differential extinction risk) is shaped by interactions between ecological traits and environmental conditions. Numerous paleontological studies have examined trait‐based extinction selectivity; however, the extent to which these patterns are shaped by environmental conditions is poorly understood due to a lack of quantitative synthesis across studies. We conducted a meta‐analysis of published studies on fossil marine bivalves and gastropods that span 458 million years to uncover how global environmental and geochemical changes covary with trait‐based extinction selectivity. We focused on geographic range size and life habit (i.e., infaunal vs. epifaunal), two of the most important and commonly examined predictors of extinction selectivity. We used geochemical proxies related to global climate, as well as indicators of ocean acidification, to infer average global environmental conditions. Life‐habit selectivity is weakly dependent on environmental conditions, with infaunal species relatively buffered from extinction during warmer climate states. In contrast, the odds of taxa with broad geographic ranges surviving an extinction (>2500 km for genera, >500 km for species) are on average three times greater than narrow‐ranging taxa (estimate of odds ratio: 2.8, 95% confidence interval = 2.3–3.5), regardless of the prevailing global environmental conditions. The environmental independence of geographic range size extinction selectivity emphasizes the critical role of geographic range size in setting conservation priorities.     

Pyridine nucleotide levels and activities of dehydrogenases in cambial derivatives ofRobinia pseudoacacia L.

Despite the importance of the vascular cambial differentiation, little is known about its regulation. In order to address this problem we attempted to biochemically characterize differentiating xylem and phloem elements during the early stages of development. By applying techniques of quantitative histochemistry we show that the total pool size of pyridine nucleotides is similar in the phloem (PD) and xylem (XD) oriented derivatives of the cambial zone of trees ofRobinia pseudoacacia L. Within the PD zone, the amount of NAD + NADH exceeded that of NADP + NADPH [around 600 versus 200 pmol (mg dry weight)^-1], possibly indicative of a preponderance of catabolic pathways (ratio of NADH∶NAD about 1). In contrast, the NADP(H) system dominated in the XD zone. This coincided with a high activity of NAD kinase. In addition, the extractable activities of the key enzymes of the oxidative pentose phosphate pathway, glucose-6-phosphate dehydrogenase and 6-phosphogluconate dehydrogenase, were greatly increased. At a ratio of NADPH∶NADP of approximately 1, this could be indicative of increased rates of reductive biosyntheses, and could thus well be involved in early steps of the formation of phenols and lignin monomers. Taken together, this first approach clearly shows that phloem-oriented and xylem-oriented cambial descendents exhibit distinct differences in their biochemical patterns even in early stages of differentiation.     

Munc-18–1 and cysteine string protein (csp) in pinealocytes of the gerbil pineal gland

Mammalian pinealocytes contain several synaptic membrane proteins which probably play a role in the targeting and exocytosis of secretory vesicles, in particular of synaptic-like microvesicles (SLMVs). The latter are considered as the endocrine equivalent of neuronal synaptic vesicles. By means of immunocytochemical techniques and immunoblot analyses, we now show that two further key components of the molecular apparatus regulating neurotransmitter release are present in the gerbil pineal gland, i.e., munc-18–1 and cysteine string protein (csp). In addition to varicosities of nerve fibres, munc-18–1 and csp could be localized to pinealocytes where both proteins were markedly enriched in process swellings. When using antibodies against csp for an immunogold electron-microscopic study of pinealocytes, gold particles consistently decorated profiles of pleomorphic SLMVs. Interestingly, we found that also the cytosolic protein munc-18, which is partially recruited to the plasmalemma in neurons, was associated to a significant extent with SLMVs of pinealocytes and synaptic vesicles of neurons, respectively. This localization implies that munc-18 at least partially exerts its regulatory functions while being bound to secretory vesicle membranes. Our results indicate that in endocrine cells such as pinealocytes the synaptic proteins munc-18–1 and csp play essential roles during the life cycle of SLMVs.     

The signal peptide of the ebolavirus glycoprotein influences interaction with the cellular lectins DC-SIGN and DC-SIGNR

The C-type lectins DC-SIGN and DC-SIGNR (collectively referred to as DC-SIGN/R) bind to the ebolavirus glycoprotein (EBOV-GP) and augment viral infectivity. DC-SIGN/R strongly enhance infection driven by the GP of EBOV subspecies. Zaire (ZEBOV) but have a much less pronounced effect on infection mediated by the GP of EBOV subspecies. Sudan (SEBOV). For this study, we analyzed the determinants of the differential DC-SIGN/R interactions with ZEBOV- and SEBOV-GP. The efficiency of DC-SIGN engagement by ZEBOV-GP was dependent on the rate of GP incorporation into lentiviral particles, while appreciable virion incorporation of SEBOV-GP did not allow robust DC-SIGN/R usage. Forced incorporation of high-mannose carbohydrates into SEBOV-GP augmented the engagement of DC-SIGN/R to the levels observed with ZEBOV-GP, indicating that appropriate glycosylation of SEBOV-GP is sufficient for efficient DC-SIGN/R usage. However, neither signals for N-linked glycosylation unique to SEBOV- or ZEBOV-GP nor the highly variable and heavily glycosylated mucin-like domain modulated the interaction with DC-SIGN/R. In contrast, analysis of chimeric GPs identified the signal peptide as a determinant of DC-SIGN/R engagement. Thus, ZEBOV- but not SEBOV-GP was shown to harbor high-mannose carbohydrates, and GP modification with these glycans was controlled by the signal peptide. These results suggest that the signal peptide governs EBOV-GP interactions with DC-SIGN/R by modulating the incorporation of high-mannose carbohydrates into EBOV-GP. In summary, we identified the level of GP incorporation into virions and signal peptide-controlled glycosylation of GP as determinants of attachment factor engagement.     

Regulation of the Nitrogen Transfer Pathway in the Arbuscular Mycorrhizal Symbiosis: Gene Characterization and the Coordination of Expression with Nitrogen Flux

The arbuscular mycorrhiza (AM) brings together the roots of over 80% of land plant species and fungi of the phylum Glomeromycota and greatly benefits plants through improved uptake of mineral nutrients. AM fungi can take up both nitrate and ammonium from the soil and transfer nitrogen (N) to host roots in nutritionally substantial quantities. The current model of N handling in the AM symbiosis includes the synthesis of arginine in the extraradical mycelium and the transfer of arginine to the intraradical mycelium, where it is broken down to release N for transfer to the host plant. To understand the mechanisms and regulation of N transfer from the fungus to the plant, 11 fungal genes putatively involved in the pathway were identified from Glomus intraradices, and for six of them the full-length coding sequence was functionally characterized by yeast complementation. Two glutamine synthetase isoforms were found to have different substrate affinities and expression patterns, suggesting different roles in N assimilation. The spatial and temporal expression of plant and fungal N metabolism genes were followed after nitrate was added to the extraradical mycelium under N-limited growth conditions using hairy root cultures. In parallel experiments with ¹⁵N, the levels and labeling of free amino acids were measured to follow transport and metabolism. The gene expression pattern and profiling of metabolites involved in the N pathway support the idea that the rapid uptake, translocation, and transfer of N by the fungus successively trigger metabolic gene expression responses in the extraradical mycelium, intraradical mycelium, and host plant.The arbuscular mycorrhizal (AM) symbiosis brings together the roots of the majority of land plant species and fungi of the phylum Glomeromycota to great mutual advantage (Smith and Read, 2008). AM fungi improve the acquisition of phosphate, nitrogen (N), sulfur, and trace elements such as copper and zinc (Clark and Zeto, 2000; Allen and Shachar-Hill, 2008) and increase the biotic and abiotic stress resistance of their host (Smith et al., 2010). In return, the host transfers up to 20% of its photosynthetically fixed carbon to the AM fungus (Jakobsen and Rosendahl, 1990), which depends on its host plant for its carbon supply (Bago et al., 2000).N is the nutrient whose availability most commonly limits plant growth in natural ecosystems. AM fungi can take up NO₃⁻NH₄⁺ and can also increase access to organic N sources from the soil (Ames et al., 1983; Johansen et al., 1993; Bago et al., 1996; Hodge et al., 2001). The translocation by the fungus can represent a significant route for N uptake by the plant (Johansen and Jensen, 1996). For example, Toussaint et al. (2004) showed that in an in vitro mycorrhiza at least 21% of the total N uptake in the roots came from the fungal extraradical mycelium (ERM); for other mycorrhizal systems, even larger proportions have been described (more than 30% and 50%; Govindarajulu et al., 2005; Jin et al., 2005). Tanaka and Yano (2005) reported that 75% of the N in leaves of mycorrhizal maize (Zea mays) was taken up by the ERM of Glomus aggregatum.A mechanism of N transfer from the fungus to the plant has been proposed (Bago et al., 2001) that involves the operation of a novel metabolic route in which N was translocated from the ERM to the intraradical mycelium (IRM) as Arg but transferred to the plant without carbon as inorganic N. This mechanism has been supported by labeling experiments (Johansen et al., 1996; Govindarajulu et al., 2005; Jin et al., 2005), enzyme activity analysis (Cruz et al., 2007), and limited gene expression data (Govindarajulu et al., 2005; Gomez et al., 2009; Guether et al., 2009). Nevertheless, our molecular knowledge of the metabolic and transport pathways involved and how they are regulated is still rudimentary. A better understanding of the mechanism and regulation of N uptake assimilation, translocation, and transfer to the host is important for potential applications of AM fungi as biofertilizers, bioprotectors, and bioregulators in sustainable agriculture and restoration as well as for understanding the role of AM fungi in natural ecosystems (Bruns et al., 2008).In this study, we postulate that the uptake, translocation, and transfer of N by the fungus triggers the metabolic gene expression responses successively in the ERM, IRM, and host plant, which will result in the synthesis and accumulation of Arg in the ERM, the turnover of Arg to release ammonium in the IRM, and the assimilation of ammonium by the host plant via the glutamine synthetase (GS)/glutamate synthase (GOGAT) pathway inside the root (Fig. 1). To test these predictions, 11 genes involved in the N primary assimilation and metabolism were cloned and verified from Glomus intraradices; six enzymes with full-length coding sequences (CDSs) were functionally characterized by yeast knockout mutant complementation. Two GS proteins were found to have different substrate affinities and expression patterns, suggesting that they have different roles in N assimilation. The time courses of gene expression and N movement in fungal and host tissues were analyzed following nitrate supply to the ERM of a mycorrhiza grown under N-limited conditions. The results substantially increase our knowledge of the identity and regulation of most of the metabolic and transport genes involved in N movement through the AM symbiosis.Open in a separate windowFigure 1.Working model of N transport and metabolism in the symbiosis between plant roots and arbuscular mycorrhizal fungi. N moves (black arrows) from the soil into the fungal ERM, through a series of metabolic conversion reactions into Arg, which is transported into the IRM within the root (host) and there is broken down; N is transferred to and assimilated by the host as ammonia. Red circles refer to the sites of action of the genes identified and analyzed in this study. Blue arrows indicate mechanisms hypothesized to regulate gene expression by N metabolites involved in the pathway.     

Cloning, expression, and characterization of a chitinase gene from the Antarctic psychrotolerant bacterium Vibrio sp. strain Fi:7

A marine psychrotolerant bacterium from the Antarctic Ocean showing high chitinolytic activity on chitin agar at 5 degrees C was isolated. The sequencing of the 16S rRNA indicates taxonomic affiliation of the isolate Fi:7 to the genus Vibrio. By chitinase activity screening of a genomic DNA library of Vibrio sp. strain Fi:7 in Escherichia coli, three chitinolytic clones could be isolated. Sequencing revealed, for two of these clones, the same open reading frame of 2,189 nt corresponding to a protein of 79.4 kDa. The deduced amino acid sequence of the open reading frame showed homology of 82% to the chitinase ChiA from Vibrio harveyi. The chitinase of isolate Fi:7 contains a signal peptide of 26 amino acids. Sequence alignment with known chitinases showed that the enzyme has a chitin-binding domain and a catalytic domain typical of other bacterial chitinases. The chitinase ChiA of isolate Fi:7 was overexpressed in E. coli BL21(DE3) and purified by anion-exchange and hydrophobic interaction chromatography. Maximal enzymatic activity was observed at a temperature of 35 degrees C and pH 8. Activity of the chitinase at 5 degrees C was 40% of that observed at 35 degrees C. Among the main cations contained in seawater, i.e., Na+, K+, Ca2+, and Mg2+, the enzymatic activity of ChiA could be enhanced twofold by the addition of Ca2+.