Analysis of intracellular ice nucleation in Xenopus oocytes by differential scanning calorimetry

Intracellular ice formation (IIF) plays a central role in cell damage during cryopreservation. We are investigating the factors which trigger IIF in Xenopus oocytes, with and without aquaporin water channels. Here, we report differential scanning calorimeter studies of Xenopus control oocytes which do not express aquaporins. Stage I to VI oocytes (which increase progressively in size) were investigated with emphasis on stage I and II because they are translucent and can also be studied under the cryomicroscope. Measurements were made in 1, 1.5, and 2M ethylene glycol (EG) in frog Ringers plus SnoMax. A multistep freezing protocol was used in which the samples were cooled until extracellular ice formation (EIF) occurred, partially remelted, slowly recooled through the EIF temperature, and then rapidly (10 degrees C/min) cooled. EIF in the 1, 1.5, and 2M EG occurred at -6.4, -7.8, and -8.9 degrees C, respectively. Freezing exotherms of individual stage I-VI oocytes were readily visible. A general trend was observed in which the IIF temperature of the early stage oocytes (I-III) was well below T(EIF) while the later stages (IV-VI) froze at temperatures much closer to T(EIF). Thus, in 1.5M EG, T(IIF) was -21.1, -25, and -26.6 degrees C in stages I-III, but was -17 and -8.5 degrees C for stage IV and V-VI. Concurrently, the percentage of oocytes in which IIF was observed fell dramatically from a high of 40 to 72% in early stages (I-III) to a low of only 7% in stage V-VI because, particularly in the later stages, IIF was hidden in the EIF exotherm. We conclude that early stage oocytes are a good model system in which to investigate modulators of IIF, but that late stage oocytes are damaged during EIF and infrequently supercool.     

mtDNA variation in Inuit populations of Greenland and Canada: migration history and population structure

We examined 395 mtDNA control-region sequences from Greenlandic Inuit and Canadian Kitikmeot Inuit with the aim of shedding light on the migration history that underlies the present geographic patterns of genetic variation at this locus in the Arctic. In line with previous studies, we found that Inuit populations carry only sequences belonging to haplotype clusters A2 and D3. However, a comparison of Arctic populations from Siberia, Canada, and Greenland revealed considerable differences in the frequencies of these haplotypes. Moreover, large sample sizes and regional information about birthplaces of maternal grandmothers permitted the detection of notable differences in the distribution of haplotypes among subpopulations within Greenland. Our results cast doubt on the prevailing hypothesis that contemporary Inuit trace their all of their ancestry to so-called Thule groups that expanded from Alaska about 800-1,000 years ago. In particular, discrepancies in mutational divergence between the Inuit populations and their putative source mtDNA pool in Siberia/Alaska for the two predominant haplotype clusters, A2a and A2b, are more consistent with the possibility that expanding Thule groups encountered and interbred with existing Dorset populations in Canada and Greenland.     

Invertebrate community and stream substrate responses to woody debris removal from an ice storm-impacted stream system, NY USA

We assessed the influence of ice-storm-derived debris dams on aquatic macroinvertebrates and stream substrates in a high-gradient watershed in the eastern Adirondack Mountains of New York State. Using a modification of electrofishing techniques, invertebrates were collected once before (June 2000) and once after (June 2001) wood removal from the downstream reach in each of six pairs of reaches (second and third-order streams). Stream substrates were also mapped in 2000 and 2001 to evaluate shifts in dominant substrates within a reach following wood removal. The following metrics were used to compare the invertebrate communities before and after wood removal: genera similarity, Shannon–Weiner equitability, taxa richness, dominant taxon, percent dominance and functional feeding group relative abundance. The changes in removal reaches were evaluated relative to changes in upstream reference reaches using a Before-After Control-Impact (BACI) design and analysis. Stream substrates did not change significantly in response to wood removal, although a trend toward coarser substrates was observed following removal. Following wood removal, the relative proportion of grazers increased upstream and downstream from removed dams in all streams; however, comparisons of other metrics indicated no significant response to removal. Invertebrate responses to wood removal were lower than expected, perhaps due to the presence of abundant boulder-formed pools in this high gradient system. Electronic supplementary material Electronic supplementary material is available for this article at and accessible for authorised users.     

Observations on the behavior of vitreous ice at approximately 82 and approximately 12 K

In an attempt to determine why cooling with liquid helium actually proved disadvantageous in our electron cryotomography experiments, further tests were performed to explore the differences in vitreous ice at approximately 82 and approximately 12 K. Electron diffraction patterns showed clearly that the vitreous ice of interest in biological electron cryomicroscopy (i.e., plunge-frozen, buffered protein solutions) does indeed collapse into a higher density phase when irradiated with as few as 2-3 e-/A2 at approximately 12 K. The high density phase spontaneously expanded back to a state resembling the original, low density phase over a period of hours at approximately 82 K. Movements of gold fiducials and changes in the lengths of tunnels drilled through the ice confirmed these phase changes, and also revealed gross changes in the concavity of the ice layer spanning circular holes in the carbon support. Brief warmup-cooldown cycles from approximately 12 to approximately 82 K and back, as would be required by the flip-flop cryorotation stage, did not induce a global phase change, but did allow certain local strains to relax. Several observations including the rates of tunnel collapse and the production of beam footprints suggested that the high density phase flows more readily in response to irradiation. Finally, the patterns of bubbling were different at the two temperatures. It is concluded that the collapse of vitreous ice at approximately 12 K around macromolecules is too rapid to account alone for the problematic loss of contrast seen, which must instead be due to secondary effects such as changes in the mobility of radiolytic fragments and water.     

Concentration-dependent oligomerization and oligomeric arrangement of LptA

Gram-negative bacteria such as Escherichia coli have an inner membrane and an asymmetric outer membrane (OM) that together protect the cytoplasm and act as a highly selective permeability barrier. Lipopolysaccharide (LPS) is the major component of the outer leaflet of the OM and is essential for the survival of nearly all Gram-negative bacteria. Recent advances in understanding the proteins involved in the transport of LPS across the periplasm and into the outer leaflet of the OM include the identification of seven proteins suggested to comprise the LPS transport (Lpt) system. Crystal structures of the periplasmic Lpt protein LptA have recently been reported and show that LptA forms oligomers in either an end-to-end arrangement or a side-by-side dimer. It is not known if LptA oligomers bridge the periplasm to form a large, connected protein complex or if monomeric LptA acts as a periplasmic shuttle to transport LPS across the periplasm. Therefore, the studies presented here focus specifically on the LptA protein and its oligomeric arrangement and concentration dependence in solution using experimental data from several biophysical approaches, including laser light scattering, crosslinking, and double electron electron resonance spectroscopy. The results of these complementary techniques clearly show that LptA readily associates into stable, end-to-end, rod-shaped oligomers even at relatively low local protein concentrations and that LptA forms a continuous array of higher order oligomeric end-to-end structures as a function of increasing protein concentration.     

Methanogenic potential of Arctic and Antarctic subglacial environments with contrasting organic carbon sources

Subglacial environments are largely anoxic, contain organic carbon (OC) overridden by glacier ice during periods of advance, and harbour active microbial communities. This creates favourable conditions for OC degradation via methanogenesis. It has been hypothesized that OC beneath ice sheets is converted to methane (CH₄) and may be released to the atmosphere during retreat. However, there are limited data available to support this contention. Here, we present new data on the abundance, diversity and activity of methanogenic archaea and the amount and character of OC in subglacial sediments from Arctic and Antarctic glacial systems based on different substrate types. We employed long‐term laboratory incubations to quantify the CH₄ production potential in different subglacial settings. Significant numbers of methanogens (up to 7 × 10⁴ cells g^?1) were detected in the samples and clones of Methanomicrobiales and Methanosarcinales were identified in clone libraries. Long lag periods (up to >200 days) were observed before significant CH₄ concentrations were measured. We report order of magnitude differences in rates of CH₄ production (10¹–10⁵ fmol g^?1 d^?1) in different subglacial sediments, reflecting contrasts in the origin of the sediment and the OC character. Hence, we predict that contrasting rates of CH₄ production are likely to occur beneath glaciers and ice sheets that overran different types of substrate. We subsequently estimated the potential for CH₄ production beneath the Laurentide/Inuitian/Cordilleran and Fennoscandian Ice Sheets during a typical 85 ka Quaternary glacial/interglacial cycle. CH₄ production from lacustrine‐derived OC is likely to be an order of magnitude higher (~6.3–27 Pg C) than that from overridden soils (~0.55–0.68 Pg C), possibly due to a difference in lability between lacustrine and soil OC. While representing a fraction of the entire OC pool (~418–610 Pg C), this finding highlights the importance of considering the character of different OC pools when calculating subglacial CH₄ production.     

Effects of climate change on an emperor penguin population: analysis of coupled demographic and climate models

Sea ice conditions in the Antarctic affect the life cycle of the emperor penguin (Aptenodytes forsteri). We present a population projection for the emperor penguin population of Terre Adélie, Antarctica, by linking demographic models (stage‐structured, seasonal, nonlinear, two‐sex matrix population models) to sea ice forecasts from an ensemble of IPCC climate models. Based on maximum likelihood capture‐mark‐recapture analysis, we find that seasonal sea ice concentration anomalies (SIC_a) affect adult survival and breeding success. Demographic models show that both deterministic and stochastic population growth rates are maximized at intermediate values of annual SIC_a, because neither the complete absence of sea ice, nor heavy and persistent sea ice, would provide satisfactory conditions for the emperor penguin. We show that under some conditions the stochastic growth rate is positively affected by the variance in SIC_a. We identify an ensemble of five general circulation climate models whose output closely matches the historical record of sea ice concentration in Terre Adélie. The output of this ensemble is used to produce stochastic forecasts of SIC_a, which in turn drive the population model. Uncertainty is included by incorporating multiple climate models and by a parametric bootstrap procedure that includes parameter uncertainty due to both model selection and estimation error. The median of these simulations predicts a decline of the Terre Adélie emperor penguin population of 81% by the year 2100. We find a 43% chance of an even greater decline, of 90% or more. The uncertainty in population projections reflects large differences among climate models in their forecasts of future sea ice conditions. One such model predicts population increases over much of the century, but overall, the ensemble of models predicts that population declines are far more likely than population increases. We conclude that climate change is a significant risk for the emperor penguin. Our analytical approach, in which demographic models are linked to IPCC climate models, is powerful and generally applicable to other species and systems.     

Southern Ocean Biogeography of Tintinnid Ciliates of the Marine Plankton

Ciliate microzooplankton are important grazers in most pelagic ecosystems and among them, tintinnids, with their largely species‐specific loricas, allow relatively easy assessment of questions of diversity and distributions. Herein, we present the results of a survey of species records of tintinnids from the Southern Ocean (locations below 40°S) reported in 56 publications yielding 2,047 species records (synonyms included) from 402 locations. The 192 species reported can be parsed into two main groups: 32 endemic Southern Ocean species, known only from 40°S and further south, and a second group of 181 widespread species, forms with extensive geographic ranges extending into the Southern Ocean. Widespread species reported from the Southern Ocean can be further divided into a group of 81 species, each recorded multiple times in the Southern Ocean waters and 70 apparent “stray” species which have only been found but once. The endemic and widespread species of the Southern Ocean show both distinct distributional patterns and morphological differences. The assemblage of Southern Ocean endemics is found mostly within the Antarctic zone delimited by the average location of the Polar Front and contains a relatively large portion of wide‐mouthed forms. We give suggestions for future study.     

Conformational change from antiparallel beta-sheet to alpha-helix in a series of depsipeptide, -(Leu-Leu-Lac)(n)-: syntheses, spectroscopic studies, and crystal structures of Boc-Leu-Lac-OEt and Boc-(Leu-Leu-Lac)(n)-OEt (n = 1, 2)

The depsipeptides Boc-Leu-Lac-OEt (1) and Boc-(Leu-Leu-Lac)(n)-OEt (n = 1, 2) (2 and 3, respectively) (Boc = tert-butyloxycarbonyl, Lac = L-lactic acid residue) has been synthesized and studied by crystallographic, CD spectroscopic, and ESI-MS analyses. In the packing cells, those three compounds adopt beta-strand conformations. Each molecule is linked into a dimer (1) or an infinite assembly (2 and 3) by tight hydrogen bonds of the type NH...O==C. Interestingly, the hexamer, 3 shows the first example of antiparallel pleated beta-sheet crystal structure for a depsipeptide molecule. In the packing cells, especially for 3, the ester groups O--C==O are perpendicularly oriented to the amide groups NH--C==O and beta-sheet planes to avoid the interaction between --O--(ester) and O==C. Therefore, when the chain length become longer, the O...O==C repulsion interaction works as a beta-sheet breaker and hence promotes an alpha-helical structure as observed for Boc-(Leu-Leu-Lac)(3)-Leu-Leu-OEt (4) (Oku et al. Biopolymers 2004, 75, 242-254) and Boc-(Leu-Leu-Lac)(n)-OEt (n = 4-6) (5-7) (Katakai et al., Biopolymers 1996, 38, 285-290), in which the O...O==C repulsion does not cause significant structural changes in alpha-helical main chains. Therefore from the structural and spectroscopic analyses, we have found governing factors for the specificity in the beta-sheet and alpha-helix decision in this series of depsipeptides, -(Leu-Leu-Lac)(n)-.