Evidence of enhanced freezing damage in treeline plants during six years of CO2 enrichment and soil warming

Climate change and elevated atmospheric CO₂ levels could increase the vulnerability of plants to freezing. We analyzed tissue damage resulting from naturally occurring freezing events in plants from a long–term in situ CO₂ enrichment (+ 200 ppm, 2001–2009) and soil warming (+ 4°C since 2007) experiment at treeline in the Swiss Alps (Stillberg, Davos). Summer freezing events caused damage in several abundant subalpine and alpine plant species in four out of six years between 2005 and 2010. Most freezing damage occurred when temperatures dropped below –1.5°C two to three weeks after snow melt. The tree Larix decidua and the dwarf shrubs Vaccinium myrtillus and Empetrum hermaphroditum showed more freezing damage under experimentally elevated CO₂ and/or temperatures than under control conditions. Soil warming induced a 50% die‐back of E. hermaphroditum during a single freezing event due to melting of the protective snow cover. Although we could not identify a clear mechanism, we relate greater freezing susceptibility to a combination of advanced plant phenology in spring and changes in plant physiology. The climate record since 1975 at the treeline site indicated a summer warming by 0.58°C/decade and a 3.5 days/decade earlier snow melt, but no significant decrease in freezing events during the vegetation period. Therefore, in a warmer climate with higher CO₂ levels but constant likelihood of extreme weather events, subalpine and alpine plants may be more susceptible to freezing events, which may partially offset expected enhanced growth with global change. Hence, freezing damage should be considered when predicting changes in growth of alpine plants or changes in community composition under future atmospheric and climate conditions.     

Analysis of goldenseal, Hydrastis canadensis L., and related alkaloids in urine using HPLC with UV detection

A screening method was developed to extract and detect berberine and hydrastine alkaloids from goldenseal root powder and urine samples using HPLC with UV detection. The isocratic method was developed to detect alkaloids in 5 mL of urine prior to drug screening. Urine samples were spiked with the alkaloids at varying concentrations and extracted twice with 3:1 chloroform:2-propanol (CHCl(3):2-propanol). The extracts were combined, concentrated using nitrogen gas and the residue was then reconstituted with a mobile phase of acetonitrile:buffer (32:68). A 17 min isocratic run time was performed with a flow rate of 2.0 mL/min, and UV detection at 230 nm using a C(18) (250 mm × 4.6 mm) column at room temperature. The method showed good linearity for berberine (r(2)=0.9990) and hydrastine (r(2)=0.9983) over a range of 11.80 ng/mL to 17.64 μg/mL. The LOD for berberine in urine was 12.74 ng/mL and the LOD for hydrastine in urine was 54.48 ng/mL. Urine samples were spiked with goldenseal root powder and liquid extract as part of a blinded study to determine whether berberine and hydrastine alkaloids could also be extracted in vitro from goldenseal and show a presence in urine samples. Out of the 37 blinded urine samples extracted the two spiked samples were correctly identified based on the presence or absence of berberine and hydrastine. The results demonstrated that this method will enable laboratories to test for the herbal supplement in submitted urine samples prior to drug testing, avoiding false negative results.     

Reactive oxygen species and yeast apoptosis

Apoptosis is associated in many cases with the generation of reactive oxygen species (ROS) in cells across a wide range of organisms including lower eukaryotes such as the yeast Saccharomyces cerevisiae. Currently there are many unresolved questions concerning the relationship between apoptosis and the generation of ROS. These include which ROS are involved in apoptosis, what mechanisms and targets are important and whether apoptosis is triggered by ROS damage or ROS are generated as a consequence or part of the cellular disruption that occurs during cell death. Here we review the nature of the ROS involved, the damage they cause to cells, summarise the responses of S. cerevisiae to ROS and discuss those aspects in which ROS affect cell integrity that may be relevant to the apoptotic process.     

PHYLOGENETIC ANALYSIS OF THE LARGE SUBUNIT RUBISCO GENE SUPPORTS THE EXCLUSION OF AVRAINVILLEA AND CLADOCEPHALUS FROM THE UDOTEACEAE (BRYOPSIDALES,CHLOROPHYTA)1

The placement of Avrainvillea and Cladocephalus in the family Udoteaceae (order Bryopsidales) has been questioned on the basis of nuclear, plastid, and other ultrastructural characteristics unique to these genera. Bayesian analysis of the chloroplast‐encoded LSU RUBISCO (rbcL) gene showed that the Udoteaceae is paraphyletic. Cladocephalus luteofuscus (P. Crouan et H. Crouan) Børgesen, Avrainvillea nigricans f. floridana D. Littler et Littler, and A. mazei G. Murray et Boodle form a clade with the freshwater alga Dichotomosiphon tuberosus (A. Braun ex Kütz.) A. Ernst that is basal to a clade that includes other members of the Udoteaceae, the Halimedaceae, and the Caulerpaceae. The noncalcified species Boodleopsis pusilla (Collins) W. R. Taylor, A. B. Joly et Bernat. groups with species of the calcified Udoteacean genera Penicillus, Rhipocephalus, Udotea, and Halimeda.     

Soil warming opens the nitrogen cycle at the alpine treeline

Climate warming may alter ecosystem nitrogen (N) cycling by accelerating N transformations in the soil, and changes may be especially pronounced in cold regions characterized by N‐poor ecosystems. We investigated N dynamics across the plant–soil continuum during 6 years of experimental soil warming (2007–2012; +4 °C) at a Swiss high‐elevation treeline site (Stillberg, Davos; 2180 m a.s.l.) featuring Larix decidua and Pinus uncinata. In the soil, we observed considerable increases in the pool size in the first years of warming (by >50%), but this effect declined over time. In contrast, dissolved organic nitrogen (DON) concentrations in soil solutions from the organic layer increased under warming, especially in later years (maximum of +45% in 2012), suggesting enhanced DON leaching from the main rooting zone. Throughout the experimental period, foliar N concentrations showed species‐specific but small warming effects, whereas δ¹⁵N values showed a sustained increase in warmed plots that was consistent for all species analysed. The estimated total plant N pool size at the end of the study was greater (+17%) in warmed plots with Pinus but not in those containing Larix, with responses driven by trees. Irrespective of plot tree species identity, warming led to an enhanced N pool size of Vaccinium dwarf shrubs, no change in that of Empetrum hermaphroditum (dwarf shrub) and forbs, and a reduction in that of grasses, nonvascular plants, and fine roots. In combination, higher foliar δ¹⁵N values and the transient response in soil inorganic N indicate a persistent increase in plant‐available N and greater cumulative plant N uptake in warmer soils. Overall, greater N availability and increased DON concentrations suggest an opening of the N cycle with global warming, which might contribute to growth stimulation of some plant species while simultaneously leading to greater N losses from treeline ecosystems and possibly other cold biomes.     

The Asian red seaweed <Emphasis Type="Italic">Grateloupia turuturu</Emphasis> (Rhodophyta) invades the Gulf of Maine

We report the invasion of the Gulf of Maine, in the northwest Atlantic Ocean, by the largest red seaweed in the world, the Asian Grateloupia turuturu. First detected in 1994 in Narragansett Bay, Rhode Island, south of Cape Cod, this alga had expanded its range in the following years only over to Long Island and into Long Island Sound. In July 2007 we found Grateloupia in the Cape Cod Canal and as far north (east) as Boston, Massachusetts, establishing its presence in the Gulf of Maine. Grateloupia can be invasive and may be capable of disrupting low intertidal and shallow subtidal seaweeds. The plant's broad physiological tolerances suggest that it will be able to expand possibly as far north as the Bay of Fundy. We predict its continued spread in North America and around the world, noting that its arrival in the major international port of Boston may now launch G. turuturu on to new global shipping corridors.     

The onset of oscillatory dynamics in models of multiple disease strains

 We examine a generalised SIR model for the infection dynamics of four competing disease strains. This model contains four previously-studied models as special cases. The different strains interact indirectly by the mechanism of cross-immunity; individuals in the host population may become immune to infection by a particular strain even if they have only been infected with different but closely related strains. Several different models of cross-immunity are compared in the limit where the death rate is much smaller than the rate of recovery from infection. In this limit an asymptotic analysis of the dynamics of the models is possible, and we are able to compute the location and nature of the Takens–Bogdanov bifurcation associated with the presence of oscillatory dynamics observed by previous authors. Received: 5 December 2001 / Revised version: 5 May 2002 / Published online: 17 October 2002 Keywords or phrases: Infection – Pathogen – Epidemiology – Multiple strains – Cross-immunity – Oscillations – Dynamics – Bifurcations