A High Arctic soil ecosystem resists long‐term environmental manipulations

We evaluated above‐ and belowground ecosystem changes in a 16 year, combined fertilization and warming experiment in a High Arctic tundra deciduous shrub heath (Alexandra Fiord, Ellesmere Island, NU, Canada). Soil emissions of the three key greenhouse gases (GHGs) (carbon dioxide, methane, and nitrous oxide) were measured in mid‐July 2009 using soil respiration chambers attached to a FTIR system. Soil chemical and biochemical properties including Q₁₀ values for CO₂, CH₄, and N₂O, Bacteria and Archaea assemblage composition, and the diversity and prevalence of key nitrogen cycling genes including bacterial amoA, crenarchaeal amoA, and nosZ were measured. Warming and fertilization caused strong increases in plant community cover and height but had limited effects on GHG fluxes and no substantial effect on soil chemistry or biochemistry. Similarly, there was a surprising lack of directional shifts in the soil microbial community as a whole or any change at all in microbial functional groups associated with CH₄ consumption or N₂O cycling in any treatment. Thus, it appears that while warming and increased nutrient availability have strongly affected the plant community over the last 16 years, the belowground ecosystem has not yet responded. This resistance of the soil ecosystem has resulted in limited changes in GHG fluxes in response to the experimental treatments.     

Aircraft‐derived regional scale CO2 fluxes from vegetated drained thaw‐lake basins and interstitial tundra on the Arctic Coastal Plain of Alaska

The landscape surface of the Barrow Peninsula of Alaska is a mosaic of small ponds, thaw lakes, different aged vegetated drained thaw‐lake basins (VDTLBs), and interstitial tundra which have been dynamically formed by both short‐ and long‐term processes. We used a combination of tower‐ and aircraft‐based eddy covariance measurements to characterize the spatial and temporal patterns of CO₂, latent, and sensible heat fluxes along with MODIS NDVI, and were able to scale the aircraft‐based CO₂ fluxes to the 1802 km² Barrow Peninsula region. During typical 2006 summer conditions, the midday hourly CO₂ flux over the region was ?2.04 × 10⁵ kg CO₂ h^?1. The CO₂ fluxes among the interstitial tundra, Ancient, and Old VDTLBs, as well as between the Medium and Young VDTLBs were not significantly different. Combined, the interstitial tundra and Old and Ancient VDTLBs represent～67% of the Barrow Peninsula surface area, accounting for ～59% of the regional flux signal. Although the Medium and Young VDTLBs represent ～11% of the surface area, they account for a large portion, ～35%, of the total regional flux. The remaining ～22% of the surface area are lakes and contributed the remaining ～6% of the total regional flux. Previous studies treated vegetated areas of the region as a single surface type with measurements from a few study sites; doing so could underestimate the regional flux by ～22%. Here, we demonstrate that aircraft‐based systems have the ability to cover large spatial scales while measuring the turbulent fluxes across a number of surfaces and combined with ground‐ and satellite‐based measurements provide a valuable tool for both scaling and validation of regional‐scale fluxes.     

Changes in high arctic tundra plant reproduction in response to long‐term experimental warming

We provide new information on changes in tundra plant sexual reproduction in response to long‐term (12 years) experimental warming in the High Arctic. Open‐top chambers (OTCs) were used to increase growing season temperatures by 1–2 °C across a range of vascular plant communities. The warming enhanced reproductive effort and success in most species; shrubs and graminoids appeared to be more responsive than forbs. We found that the measured effects of warming on sexual reproduction were more consistently positive and to a greater degree in polar oasis compared with polar semidesert vascular plant communities. Our findings support predictions that long‐term warming in the High Arctic will likely enhance sexual reproduction in tundra plants, which could lead to an increase in plant cover. Greater abundance of vegetation has implications for primary consumers – via increased forage availability, and the global carbon budget – as a function of changes in permafrost and vegetation acting as a carbon sink. Enhanced sexual reproduction in Arctic vascular plants may lead to increased genetic variability of offspring, and consequently improved chances of survival in a changing environment. Our findings also indicate that with future warming, polar oases may play an important role as a seed source to the surrounding polar desert landscape.     

Sensitivity of Siberian larch forests to climate change

The Northern Hemisphere's boreal forests, particularly the Siberian boreal forest, may have a strong effect on Earth's climate through changes in dominant vegetation and associated regional surface albedo. We show that warmer climate will likely convert Siberia's deciduous larch (Larix spp.) to evergreen conifer forests, and thus decrease regional surface albedo. The dynamic vegetation model, FAREAST, simulates Russian boreal forest composition and was used to explore the feedback between climate change and forest composition at continental, regional, and local scales. FAREAST was used to simulate the impact of changes in temperature and precipitation on total and genus‐level biomass at sites across Siberia and the Russian Far East (RFE), and for six high‐ and low‐diversity regions. Model runs with and without European Larch (Larix decidua) included in the available species pool were compared to assess the potential for this species, which is adapted to warmer climate conditions, to mitigate the effects of climate change, especially the shift to evergreen dominance. At the continental scale, when temperature is increased, larch‐dominated sites become vulnerable to early replacement by evergreen conifers. At the regional and local scales, the diverse Amur region of the RFE does not show a strong response to climate change, but the low‐diversity regions in central and southern Siberia have an abrupt vegetation shift from larch‐dominated forest to evergreen‐conifer forest in response to increased temperatures. The introduction of L. decidua prevents the collapse of larch in these low‐diversity areas and thus mitigates the response to warming. Using contemporary MODIS albedo measurements, we determined that a conversion from larch to evergreen stands in low‐diversity regions of southern Siberia would generate a local positive radiative forcing of 5.1±2.6 W m^?2. This radiative heating would reinforce the warming projected to occur in the area under climate change.     

Evidence from mitochondrial genomics supports the lower Mesozoic of South Asia as the time and place of basal divergence of cypriniform fishes (Actinopterygii: Ostariophysi)

We analysed mitochondrial genomic sequences under maximum likelihood (ML) criteria to explore phylogenetic relationships, and performed historical biogeography analysis with divergence time estimation for fishes of Order Cypriniformes (Actinopterygii: Ostariophysi). We added mitogenomes for eight new cypriniforms and one outgroup to a data set comprising 53 and six outgroup mitogenomes from a previous study to make our taxon sampling geographically representative. The ML tree reconfirmed monophyly of four basal cypriniform clades (cyprinids, catostomids, gyrinocheilids, and loaches including balitorids and cobitids). It also recovered 18 monophyletic groups largely equivalent to the subfamilial rank, and resolved interrelationships among most of these subfamilial clades. However, lower bootstrap support for the ML tree and higher approximately unbiased (au) probabilities for alternative topologies around some branches indicated problems that still need to be resolved. Historical taxon biogeography by dispersal‐vicariance analysis, a parsimonious reconstruction of past ranges, and gain‐loss ratio analysis at the subfamilial level, identified the geographical region of basal cypriniform divergence as southern Asia. Bayesian divergence time analysis dated the basal otophysan split, which gave birth to Order Cypriniformes, to the late Triassic around 219.5 Mya. The basal cypriniform divergence took place during the late Jurassic around 155.9 Mya. These dates coincide with the onset and completion, respectively, of the Pangaean breakup. Taking biogeographical analysis and node dating into account, we consider the most likely candidate for the initial geographical range of Order Cypriniformes to be the south‐eastern area of Mesozoic Laurasia (present‐day southern Asia, excluding the Indian subcontinent). We also briefly discuss ecological implications of the group's divergence. © 2011 The Linnean Society of London, Zoological Journal of the Linnean Society, 2011, 161 , 633–662.     

Night and day: short‐term variation in nitrogen chemistry and nitrous oxide emissions from streams

1. Diel variation in metabolism contributes to variation in oxygen (O₂) concentrations in streams. This variation in O₂ and other parameters (e.g. pH) can in turn affect the rates of microbial nitrogen (N) processing, concentrations of nitrogenous solutes and production of the greenhouse gas nitrous oxide (N₂O). We investigated diel variability in emissions of N₂O and the magnitude of short‐term variability in N solutes across 10 streams. 2. Nitrous oxide fluxes varied on average 2.3‐fold over diel cycles. Concentrations would be underestimated by sampling around noon, but N₂O fluxes would not show a consistent bias. Time‐weighted mean daily N₂O flux was strongly related to nitrate concentration (r² = 0.58). Diel patterns in N₂O and dissolved N species were often complex (rather than simple sinusoidal curves), probably reflecting complex underlying processes. 3. Reliance on samples obtained around noon would overestimate daily mean nitrate concentrations by 5% and underestimate ammonium by 32% (average bias across all streams and dates). 4. Dissolved organic N did not show consistent day–night variation. However, the magnitude of diel variability was similar to that observed for dissolved inorganic N. Organic and inorganic N concentrations were often similar. Both appear to be dynamic components of stream N budgets. 5. The Intergovernmental Panel on Climate Change (IPCC) relies upon an emission factor to estimate indirect agricultural N₂O emissions from streams and ground water. The measured emission factor (defined as the ratio of concentrations of N₂O‐N to ‐N) was typically below the recently revised IPCC default figure. Measured values varied on average 1.8‐fold over approximately 24‐h periods and were slightly higher at night than by day. The emission factor was actually highest in streams that were net sinks for N₂O, highlighting a conceptual problem in the current IPCC method. 6. Typical sampling programmes rely on daytime‐only sampling, which might cause bias in results. In our study streams, the bias was generally small. Diel variation in nitrate concentrations was related to mean temperature; variation in ammonium and N₂O concentrations was greatest at low concentrations of nitrite and ammonium.     

Climate impacts on Mediterranean blue tit survival: an investigation across seasons and spatial scales

In some hole nesting passerine species, long‐term monitoring data are available for several geographically independent populations. Climate forcing can then be documented and predictions made on the scale of distribution ranges. Several demographic studies of Paridae report dramatic impacts of wintertime climatic factors. However, these studies were undertaken in populations located in the northern parts of the species' ranges. Studies on the survival of Paridae in their southern ranges are necessary in order to assess potential latitudinal variation in climate forcing on survival. Based on monitoring of individual adult blue tits (Parus caeruleus), the effects of climatic factors on annual survival were assessed in three distinct Mediterranean populations. In these regions, climatic conditions in early summer might be expected to have a strong impact because they can be extremely hot and dry and because at this time of year Paridae are subjected to intrinsic constraints that stem from energetically costly postbreeding moult, recovery from reproductive costs, and from population densities inflated by the new cohort of fledglings. The impact of climatic conditions in early summer was, thus, addressed in addition to that prevailing in winter. In order to consider a large number of local climatic variables while limiting statistical power loss, integrative indices of local climate were built using multivariate techniques. In addition, the NAO and three large‐scale factors that are closely linked with atmospheric and oceanic circulation in the intertropical zone were considered as potentially influential factors in winter and early summer. Relationships between blue tit survival and indices of local temperature and precipitation in winter and in early summer were detected. Adult survival also correlated with a large‐scale tropical index in early summer: rainfall in the Sahel. This is one of the first quantitative indications that fluctuations in summer climatic conditions explain a significant part of the temporal variation in adult survival in unconnected populations of a sedentary European vertebrate. Furthermore, the results support the hypothesis that summertime local climates in Western Europe are closely linked with atmospheric and oceanic circulation in the intertropical zone.     

BIOCHEMICAL DETECTION AND IMMUNOHISTOCHEMICAL LOCALIZATION OF ENKEPHALIN-LIKE SUBSTANCES IN PERIPHERAL TISSUES OF THE SCALLOP PECTEN MAXIMUS (LINNAEUS)

This study focused on the biochemical detection of the methionine-enkephalin-,leucine-enkephalin-and methionine-enkephalin-arg-gly-leu-likepeptides in the stomach, digestive gland, male and female gonads,muscle, gill and mantle of the scallop Pecten maximus usingspecific radioimmunoassays. Enkephalin-like substances weremainly present in the stomach and in the digestive gland, whereleucine-enkephalin-and methionine-enkephalin-arg-gly-leu-likepeptides were the predominant of these substances. In the gonads,muscle, gill and mantle, the enkephalin-like contents were closeto the sensitivity threshold of the enkephalin antibodies. Theenkephalin-like contents measured in September, in the digestivecomplex, were significantly higher than in December, when thebivalves have undergone a period of starvation. Immunohistochemicalassays were performed on the stomach and the digestive glandto localize the enkephalin-like materials. In these organs,which are the main sites of the digestive process in Bivalyia,the enkephalin-like materials were mainly confined to the endocrine-likecells. These results suggest that in Pecten maximus, opioidsmay be involved in the digestive processes mainly through enkephalin-endocrine-likecells. (Received 29 December 1994; accepted 1 May 1995)     

Chrysoperla lucasina (Lacroix): a distinct species of green lacewing, confirmed by acoustical analysis (Neuroptera: Chrysopidae)

The existence of cryptic, sibling species, distinguished principally by vibrational courtship songs, has been confirmed for the carnea -group of Chrysoperla green lacewings in Europe and western Asia. One member of this species-group, C.lucasina (Lacroix), is characterized by several morphological traits as well, but its taxonomic validity has been considered uncertain due to the subtle and variable nature of those traits. Here, we describe the calling and courtship songs of C.lucasina , which uniquely distinguish that taxon from all other members of the carnea -group in Europe. The male of C.lucasina produces two slightly but consistently different types of songs, one while calling and the other while dueting with a female. The female produces just one type of song, identical to the male's calling song, which is used for both calling and dueting. Measured features of the songs of C.lucasina are nearly invariant over a broad geographical area, from the Canary Islands to Cyprus and from northern Africa to the U.K. Similarly, at least one morphological feature, the presence of a dark stripe on the pleuron of the second abdominal segment, characterizes all adult individuals identified acoustically as C.lucasina . Furthermore, larval head markings vary little among different populations of the song species. We conclude that C.lucasina is a valid biological species, which can also be recognized in museum collections by a suite of morphological attributes. We also briefly compare the songs and adult morphology of C.lucasina with five other currently unnamed song species of the carnea -group whose geographic ranges overlap extensively with it.