Past and present distribution, densities and movements of blue whales Balaenoptera musculus in the Southern Hemisphere and northern Indian Ocean

• 1 Blue whale locations in the Southern Hemisphere and northern Indian Ocean were obtained from catches (303 239), sightings (4383 records of ≥8058 whales), strandings (103), Discovery marks (2191) and recoveries (95), and acoustic recordings.
• 2 Sighting surveys included 7 480 450 km of effort plus 14 676 days with unmeasured effort. Groups usually consisted of solitary whales (65.2%) or pairs (24.6%); larger feeding aggregations of unassociated individuals were only rarely observed. Sighting rates (groups per 1000 km from many platform types) varied by four orders of magnitude and were lowest in the waters of Brazil, South Africa, the eastern tropical Pacific, Antarctica and South Georgia; higher in the Subantarctic and Peru; and highest around Indonesia, Sri Lanka, Chile, southern Australia and south of Madagascar.
• 3 Blue whales avoid the oligotrophic central gyres of the Indian, Pacific and Atlantic Oceans, but are more common where phytoplankton densities are high, and where there are dynamic oceanographic processes like upwelling and frontal meandering.
• 4 Compared with historical catches, the Antarctic (‘true’) subspecies is exceedingly rare and usually concentrated closer to the summer pack ice. In summer they are found throughout the Antarctic; in winter they migrate to southern Africa (although recent sightings there are rare) and to other northerly locations (based on acoustics), although some overwinter in the Antarctic.
• 5 Pygmy blue whales are found around the Indian Ocean and from southern Australia to New Zealand. At least four groupings are evident: northern Indian Ocean, from Madagascar to the Subantarctic, Indonesia to western and southern Australia, and from New Zealand northwards to the equator. Sighting rates are typically much higher than for Antarctic blue whales.
• 6 South‐east Pacific blue whales have a discrete distribution and high sighting rates compared with the Antarctic. Further work is needed to clarify their subspecific status given their distinctive genetics, acoustics and length frequencies.
• 7 Antarctic blue whales numbered 1700 (95% Bayesian interval 860–2900) in 1996 (less than 1% of original levels), but are increasing at 7.3% per annum (95% Bayesian interval 1.4–11.6%). The status of other populations in the Southern Hemisphere and northern Indian Ocean is unknown because few abundance estimates are available, but higher recent sighting rates suggest that they are less depleted than Antarctic blue whales.

     

The ecology and agronomy of Miscanthus sinensis, a species important to bioenergy crop development, in its native range in Japan: a review

Among several candidate perennial taxa, Miscanthus × giganteus has been evaluated and promoted as a promising bioenergy crop. Owing to several limitations, however, of the sterile hybrid, both at the taxon and agronomic production levels, other options need to be explored to not only improve M . × giganteus , which was originally collected in Japan, but to also consider the development of other members of its genus, including Miscanthus sinensis , as bioenergy crops. Indeed, there is likely much to be learned and applied to Miscanthus as a bioenergy crop from the long history of intensive interaction between humans and M. sinensis in Japan, which in some regions of the country spans several thousand years. Combined with its high amount of genetic variation, stress tolerance, biotic interactions with fauna, and function as a keystone species in diverse grasslands and other ecosystems within its native range, the unique and extensive management of M. sinensis in Japan as a forage grass and building material provides agronomists, agroecologists, and plant breeders with the capability of better understanding this species in terms of potential contribution to bioenergy crop development. Moreover, the studies described in this review may serve as a platform for future research of Miscanthus as a bioenergy crop in other parts of the world.     

Aboveground plant biomass,carbon, and nitrogen dynamics before and after burning in a seminatural grassland of Miscanthus sinensis in Kumamoto,Japan

Although fire has been used for several thousand years to maintain Miscanthus sinensis grasslands in Japan, there is little information about the nutrient dynamics in these ecosystems immediately after burning. We investigated the loss of aboveground biomass; carbon (C) and nitrogen (N) dynamics; surface soil C change before and after burning; and carbon dioxide (CO₂), methane (CH₄), and nitrous oxide (N₂O) fluxes 2 h after burning in a M. sinensis grassland in Kumamoto, Japan. We calculated average C and N accumulation rates within the soil profile over the past 7300 years, which were 58.0 kg C ha^?1 yr^?1 and 2.60 kg N ha^?1 yr^?1, respectively. After burning, 98% of aboveground biomass and litter were consumed. Carbon remaining on the field, however, was 102 kg C ha^?1. We found at least 43% of C was possibly lost due to decomposition. However, remaining C, which contained ash and charcoal, appeared to contribute to C accumulation in soil. There was no difference in the amount of 0–5 cm surface soil C before and after burning. The amount of remaining litter on the soil surface indicated burning appeared not to have caused a reduction in soil C nor did it negatively impact the sub‐surface vegetative crown of M. sinensis. Also, nearly 50 kg N ha^?1 of total aboveground biomass and litter N was lost due to burning. Compared with before the burning event, postburning CO₂ and CH₄ fluxes from soil appeared not to be directly affected by burning. However, it appears the short time span of measurements of N₂O flux after burning sufficiently characterized the pattern of increasing N₂O fluxes immediately after burning. These findings indicate burning did not cause significant reductions in soil C nor did it result in elevated CO₂ and CH₄ emissions from the soil relative to before the burning event.     

Divergent enhancer haplotype of ebony on inversion In(3R)Payne associated with pigmentation variation in a tropical population of Drosophila melanogaster

The pattern and intensity of pigmentation have direct impact on individual fitness through various ecological factors. In a Drosophila melanogaster population from southern Japan, thoracic trident pigmentation intensity of most of the strains could be classified into Dark or Light‐type. The expression level variation of the ebony gene correlated well with this phenotype and the allelic differences in expression indicated that the variation is partly due to cis‐regulatory changes. In the ～13 kb gene region, we identified 17 nucleotide sites and 2 indels that were in complete association with the thoracic trident pigmentation intensity. Interestingly, 11 out of 19 sites located within ～0.5 kb of the core epidermis enhancer. These sites had no obvious association with the abdominal pigmentation intensity in the previously analysed African populations from Uganda and Kenya, which suggested that multiple potential mutational pathways in the cis‐regulatory control region of a single gene could lead to similar phenotypic variation within this species. We also found that the Light‐type enhancer haplotype is strongly linked to a cosmopolitan inversion, In(3R)Payne, which is predominant in warmer climatic regions in both hemispheres. The sequence pattern suggested that the strong linkage may be due to selective forces related to thermal adaptation. The inferred selection for lighter pigmentation in the Japanese population is in the opposite direction of the previously reported case of selection for darker individuals in African populations. Nevertheless, both adaptive changes involved cis‐regulatory changes of ebony, which shows that this gene is likely to be a common target of natural selection.     

Carbon budget and methane and nitrous oxide emissions over the growing season in a Miscanthus sinensis grassland in Tomakomai,Hokkaido, Japan

Species in the Miscanthus genus have been proposed as biofuel crops that have potential to mitigate elevated atmospheric carbon dioxide (CO₂) levels and nitrous oxide (N₂O) and methane (CH₄) emissions. Miscanthus sinensis is widespread throughout Japan and has been used for biomass production for centuries. We assessed the carbon (C) budget and N₂O and CH₄ emissions over the growing season for 2 years in a M. sinensis‐dominated grassland that was naturally established around 1972 in Tomakomai, Hokkaido, Japan, which is near the northern limit for M. sinensis grassland establishment on Andisols. Average C budget was ?0.31 Mg C ha^?1, which indicates C was released from the grassland ecosystem to the atmosphere. Dominant components in the C budget appeared to be aboveground net primary production of plants (1.94–2.80 Mg C ha^?1) and heterotrophic respiration (2.27–3.11 Mg C ha^?1). The measurement of belowground net primary production (BNPP) of plants in the M. sinensis grassland was extremely variable, thus only an approximate value could be calculated. Mean C budget calculated with the approximated BNPP value was 1.47 and ?0.23 Mg C ha^?1 for 2008 and 2009, respectively. Given belowground biomass (9.46–9.86 Mg C ha^?1) was 3.1–6.5 times higher than that of aboveground biomass may provide additional evidence suggesting this grassland represents a C sink. Average CH₄ emissions across years of ?1.34 kg C ha^?1 would indicate this grassland acts as an atmospheric CH₄ sink. Furthermore, average N₂O emissions across years were 0.22 kg N ha^?1. While the site may contribute N₂O to the atmosphere, this value is lower compared with other grassland types. Global warming potential calculated with the approximated BNPP value was ?5.40 and 0.95 Mg CO₂ Eq ha^?1 for 2008 and 2009, respectively, and indicates this grassland could contribute to mitigation of global warming.     

Hemagglutinin-induced fusion of HAb2 and PLC cells: dynamics of fusion pore conductance

Infection of cells with influenza virus is mediated by the virus envelope protein hemagglutinin (HA) which induces fusion of viral and target membranes. Earlier we showed using fluorescent microscopy that HAb2 cells expressing HA on their plasma membranes fused with PLC cells when pH of the external medium was decreased to -5. In the present work we used double whole-cell recording to monitor the intercellular conductance in HAb2/PLC cell pairs during fusion. In approximately 40% of cell pairs the pH drop induced the intercellular conductance, which we interpret as the formation of a fusion pore. The following stages of the conductance growth were distinguished: initial fluctuations near zero (flicker), a subsequent slow increase up to 1-4 nS and a final rapid increase up to 10-100 nS (complete fusion). The first detectable intercellular conductance change (opening of a fusion pore) was accompanied by an increase in the conductances of both HAb2 and PLC cell membrane. This observation suggests that the early pore complex should be leaky. The dynamics of the intercellular conductance appeared to depend upon the voltage difference between the fusing HAb2 and PLC cells: voltages higher than 40 mV facilitated the conductance growth.     

Fragments of an Anarchist Anthropology

Fragments of an Anarchist Anthropology. David Graeber. Chicago: Prickly Paradigm Press, 2004. 105 pp.     

Effects of transmembrane gradients of bicarbonate and ammonium on junctional and nonjunctional membrane conductances in BHK cells

Weak acids are efficient blockers of gap-junctional conductance. It is generally accepted that intracellular acidification produced by weak acids fully accounts for the gap-junctional uncoupling. Protonation of the cytoplasmic portions of the channel-forming protein connexin is thought to lead to the conformational changes switching the channel from the open into the closed state. If this is the only mechanism of the weak-acid induced uncoupling, then the correlation between junctional conductance (Gj) and intracellular pH (pHin) should not depend on the means of intracellular acidification. We compared the responses of junctional conductance in BHK cells measured in double whole-cell experiments to the applied transmembrane concentration gradients of bicarbonate or ammonium. These treatments were to lower pHin in a predictable way according to the equations: pHin = pHout -lg[[HCO3]out/HCO3-]in) or pHin = PHout - lg[[NH4+]in[NH4+out), respectively. We found that the behavior of Gj depended on the substance used. At a 500-fold bicarbonate gradient (calculated pHin approximately 4.8) the cells remained coupled, while a 100- or 10-fold gradient of ammonium imposing pHin approximately 6.1 produced fast uncoupling. The responses of junctional conductance were often accompanied or preceded by changes of non-junctional membrane conductance. We suggest that the mechanisms of the weak acid/base-induced channel gating may contain an additional "lipophilic" component due to the presence of the non-dissociated form of the acid/base in cell membrane.