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Cold Conditions (cold + condition)

Distribution by Scientific Domains

Life Sciences	50%
Earth and Environmental Science	28%
Humanities and Social Sciences	21%

Selected Abstracts

Annual temperature history in Southwest Tibet during the last 400 years recorded by tree rings

INTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 7 2010
Bao Yang
Abstract We present a tree ring-width record from the southern Tibetan Plateau (TP) which spans from 1612,1998 AD (387 years). The series was developed from Tibetan juniper (Juniperus tibetica Kom) growing at sites near the western distribution limit of the species. Two versions of the chronology, a traditionally standardized chronology (TSC) and a regional curve standardization (RCS)chronology were developed. Linear regression models between ring width and mean annual temperature account for 41% (TSC) and 43% (RCS) of the annual (July,June) temperature variance for the period 1957,1998. According to the TSC reconstruction, warm periods occurred during the 1620s, 1650,1675, 1720s, 1740,1790, 1810s, 1850s,1890s, 1935,1950, and 1957,1964 and since 1980. Cold conditions prevailed during the 1630s,1640s, 1680s,1710s, 1730s, 1820,1840s, 1900s,1920s and the 1970s. Within the last 400 years, the late-20th century warming is distinctive but still within the range of natural climatic variability of this region. Comparison of our TSC reconstruction with proxy temperature records from other parts of the TP shows that the cold conditions during the 1730s, 1900s,1920s, and 1970s, and the warm periods during the 1770,1800, 1850s,1890s, 1935,1950, and 1957,1964 and since 1980 were synchronously occurring broad-scale climate anomalies on the whole TP. Differences between the reconstructions are found during the 17th century and around 1760, which were probably caused by local differences in temperature change and different sensitivity in seasonality. The RCS series portrays low-frequency variations such as warm periods during 1620,1640, 1650,1690, 1715,1790, and 1845,1875, and cold conditions during 1640,1650, 1690,1715, and 1875,1995. These long-term trends need to be verified by developing other proxy records that target to capture low-frequency signals in the future. Copyright © 2009 Royal Meteorological Society [source]

Stability of , -carotene in spray dried preparation of Rhodotorula glutinis mutant 32

JOURNAL OF APPLIED MICROBIOLOGY, Issue 3 2003
P. Bhosale
Abstract Aims: To obtain , -carotene-rich dry cell preparation from mutant 32 of Rhodotorula glutinis and determination of its pigment stability. Methods and Results: The mutant 32 of R. glutinis was grown in a 14 l stirred tank fermenter. Cell mass was concentrated 10-fold by cross-flow microfiltration and then spray dried. Butylated hydroxy toluene (BHT) and d -tocopherol were used as protecting agents. A two-level, three-variable, factorial optimization was performed to achieve moisture-free, non-viable and , -carotene-rich feed additive. Conclusions: The , -carotene and cell mass in stirred tank fermenter were found to be 54 ± 5 mg l,1 and 12·8 ± 2 g l,1, respectively. In the presence of BHT, 97 ± 3% (w/w) , -carotene was recovered for all the inlet temperatures studied. The best , -carotene and yeast powder recoveries were obtained at 160°C, 11·6% (w/v) cell mass concentration and 1 g l,1 BHT. The pigments inside dried yeast powder were stable in dark and cold condition for at least 10 weeks. The purified , -carotene got almost totally denatured, under similar conditions of storage, within 76 h. Significance and Impact of the Study: Spray dried and stable preparation of , -carotene-rich yeast, R. glutinis can provide alternative source of , -carotene for use in animal nutrition. [source]

Characterization of Arabidopsis genes involved in biosynthesis of polyamines in abiotic stress responses and developmental stages

PLANT CELL & ENVIRONMENT, Issue 11 2003
K. URANO
ABSTRACT To characterize the genes for enzymes involved in the biosynthesis of polyamines (PAs), their expression profiles were investigated and the levels of PAs in Arabidopsis thaliana quantified. In the Arabidopsis genome, eight genes involved in PAs biosynthesis were identified and the expression profiles of these genes were analysed, not only under abiotic stress to determine whether they were stress-inducible, constitutive, or stress-repressible, but also in various organs to show their tissue specificity. AtADC2 and AtSPMS mRNAs, encoding arginine decarboxylase and spermine synthase, clearly increased in response to NaCl and dehydration and abscisic acid treatments. Stress-inducible accumulation of AtADC2 mRNA correlated with putrescine (Put) accumulation under NaCl and dehydration treatments. In a cold condition, AtSAMDC2 mRNA increased significantly. AtADC2 and AtSAMDC2 mRNA were expressed in sexual organs such as flowers, buds and immature siliques. PAs also accumulated in sexual organs. These results suggest that the transcripts of eight genes involved in PA biosynthesis show different profiles of expression not only in response to environmental stress but also during plant development. [source]

A combined stress response analysis of Spirulina platensis in terms of global differentially expressed proteins, and mRNA levels and stability of fatty acid biosynthesis genes

FEMS MICROBIOLOGY LETTERS, Issue 2 2008
Wattana Jeamton
Abstract Changes in gene expression play a critical role in enhancing the ability of cyanobacteria to survive under cold conditions. In the present study, Spirulina platensis cultures were grown at the optimal growth temperature, in the light, before being transferred to dark conditions at 22 °C. Two dimensional-differential gel electrophoresis was then performed to separate differentially expressed proteins that were subsequently identified by MS. Among all differentiated proteins identified, a protein involved in fatty acid biosynthesis, (3R)-hydroxymyristoyl-[acyl-carrier-protein]-dehydratase encoded by fabZ, was the most up-regulated protein. However, the fatty-acid desaturation proteins were not significantly differentiated. This raised the question of how the unsaturated fatty acid, especially ,-linolenic acid, content in the cells in the cold,dark shift remained stable compared with that of the cold shift. Thus, a study at the transcriptional level of these desaturase genes, desC, desA and desD, and also of the fabZ gene was conducted. The results indicated that in the dark, where energy is limited, mRNA stability was enhanced by exposure to low temperatures. The data demonstrate that when the cells encounter cold stress with energy limitation, they can maintain their homeoviscous adaptation ability via mRNA stability. [source]

Multiple roles of PPAR, in brown adipose tissue under constitutive and cold conditions

GENES TO CELLS, Issue 2 2010
Makiko Komatsu
Peroxisome proliferator-activated receptor , (PPAR,) is a member of the nuclear receptor family, regulating fatty acid degradation in many organs. Two-dimensional SDS-PAGE of brown adipose tissue (BAT) from PPAR,-null mice produced a higher-density spot. Proteomic analysis indicated that the protein was pyruvate dehydrogenase , (PDH,). To observe PDH, regulation in BAT, the organ was stimulated by long-term cold exposure, and the activities of associated enzymes were investigated. Histological and biochemical analyses of BAT showed a significant decrease in the triglyceride content in wild-type mice and some degree of decrease in PPAR,-null mice on cold exposure. Analyses of molecules related to glucose metabolism showed that the expression of PDH, is under PPAR,-specific regulation, and that glucose degradation ability may decrease on cold exposure. In contrast, analyses of molecules related to fatty acid metabolism showed that numerous PPAR,/, target molecules are induced on cold exposure, and that fatty acid degradation ability in wild-type mice is markedly enhanced and also increases to same degree in PPAR,-null mice on cold exposure. Thus, this study proposes novel and multiple roles of PPAR, in BAT. [source]

Annual temperature history in Southwest Tibet during the last 400 years recorded by tree rings

Late Mousterian subsistence and cave use in Dalmatia: the zooarchaeology of Mujina Pe,ina, Croatia

INTERNATIONAL JOURNAL OF OSTEOARCHAEOLOGY, Issue 2 2005
P. Miracle
Abstract The faunal assemblage from Mujina Pe,ina provides an initial glimpse of Late Middle Palaeolithic food procurement, management, and site use, in Dalmatia, Croatia. Radiometric dates place the entire sequence at about 42,kyr in the middle of OIS 3 (Oxygen Isotope Stage 3) (Rink et al., 2002). Mujina Pe,ina is located along a potential migration corridor for hominin populations moving into Europe from western Asia. The faunal composition shifts from a co-dominance of red deer and chamois,+,ibex in Layer D1,+,D2 that formed during relatively cold conditions to a clear dominance of wild caprids followed by large bovids and equids in Layer B,+,C that formed during relatively warm conditions. Although non-hominin carnivores played a significant role in the modification of the faunal assemblages throughout the stratigraphic sequence, the Late Mousterian faunal assemblage from Mujina Pe,ina shows the hominins to be competent hunters within a context of considerable competition from non-hominin carnivores. These ,mixed' hominin-carnivore signatures are pulled apart through a detailed taphonomic analysis of this well-excavated assemblage. The Mujina Pe,ina assemblage thus provides a significant point of reference for a broader-scale study of variability in Mousterian subsistence practices in their own right as well as within the context of the Initial Upper Palaeolithic in southeastern Europe. Copyright © 2005 John Wiley & Sons, Ltd. [source]

Disturbance facilitates rapid range expansion of aspen into higher elevations of the Rocky Mountains under a warming climate

JOURNAL OF BIOGEOGRAPHY, Issue 1 2010
Simon M. Landhäusser
Abstract Aim, Trembling aspen (Populus tremuloides Michx.) is absent in the upper foothills region of west-central Alberta because of the cold conditions and short growing season at this high elevation. However, in recent years it appears that aspen has been establishing from seed in this zone and that it has been doing so mainly as a result of forest harvesting. The objectives of this study were to determine the frequency of and types of microsite required for the successful establishment of aspen seedlings at these higher elevations. Location, Rocky Mountains Upper Foothills Natural Subregion of west-central Alberta, Canada. Methods, The current distribution of mature aspen and the presence and absence of aspen seedlings in harvested areas were determined in an area c. 300 km2 in size, using ground and aerial surveys. In an intensive study, 12 belt transects (180 m long and 5 m wide) were established in areas disturbed by forest harvesting at high elevations where no aspen was present prior to harvesting. Transects were surveyed seven growing seasons after disturbance and the microsites occupied by aspen seedlings were characterized according to their substrate and microtopography. Similarly, the availability of different substrates and microtopographic positions were assessed by systematic point sampling on these sites. Results, On level surfaces, aspen seedling regeneration was found up to 200 m higher in elevation than the mature aspen in the original undisturbed forests. Overall, there were 428 seedlings ha,1 established on these transects, and the age distribution indicates that aspen seedlings had established in each of the seven growing seasons since the disturbance. Nearly all of the seedlings (93%) were established on mineral soil microsites and virtually no seedlings were established on undisturbed forest floor layers. Significantly more seedlings were found in concave microtopographic positions. Main conclusions, This study indicates that aspen establishment from seed is currently not a stochastic event and demonstrates that aspen is rapidly expanding its range upslope in the Canadian Rocky Mountain region as a result of forest management practices that expose mineral soil substrates in conjunction with a warming climate. The change in canopy composition from conifer to deciduous forests at these higher elevations will have far-reaching implications for ecosystem processes and functions. [source]

Late Quaternary deglaciation and climate history of the Larsemann Hills (East Antarctica)

JOURNAL OF QUATERNARY SCIENCE, Issue 4 2004
Elie Verleyen
Abstract The Late Quaternary climate history of the Larsemann Hills has been reconstructed using siliceous microfossils (diatoms, chrysophytes and silicoflagellates) in sediment cores extracted from three isolation lakes. Results show that the western peninsula, Stornes, and offshore islands were ice-covered between 30,000,yr,BP and 13,500,cal.,yr,BP. From 13,500,cal.,yr,BP (shortly after the Antarctic Cold Reversal) the coastal lakes of the Larsemann Hills were deglaciated and biogenic sedimentation commenced. Between 13,500 and 11,500,cal.,yr,BP conditions were warmer and wetter than during the preceding glacial period, but still colder than today. From 11,500 to 9500,cal.,yr,BP there is evidence for wet and warm conditions, which probably is related to the early Holocene climate optimum, recorded in Antarctic ice cores. Between 9500 and 7400,cal.,yr,BP dry and cold conditions are inferred from high lake-water salinities, and low water levels and an extended duration of nearshore sea-ice. A second climate optimum occurred between 7400 and 5230,cal.,yr,BP when stratified, open water conditions during spring and summer characterised the marine coast of Prydz Bay. From 5230 until 2750,cal.,yr,BP sea-ice duration in Prydz Bay increased, with conditions similar to the present day. A short return to stratified, open water conditions and a reduction in nearshore winter sea-ice extent is evident between 2750 and 2200,cal.,yr,BP. Simultaneously, reconstructions of lake water depth and salinity suggests relatively humid and warm conditions on land between 3000 and 2000,cal.,yr,BP, which corresponds to a Holocene Hypsithermal reported elsewhere in Antarctica. Finally, dry conditions are recorded around 2000, between 760 and 690, and between 280 and 140,cal.,yr,BP. These data are consistent with ice-core records from Antarctica and support the hypothesis that lacustrine and marine sediments on land can be used to evaluate the effect of long-term climate change on the terrestrial environment. Copyright © 2004 John Wiley & Sons, Ltd. [source]

Postglacial colonization of the Tibetan plateau inferred from the matrilineal genetic structure of the endemic red-necked snow finch, Pyrgilauda ruficollis

MOLECULAR ECOLOGY, Issue 6 2005
YAN HUA QU
Abstract Most phylogeographical studies of postglacial colonization focus on high latitude locations in the Northern Hemisphere. Here, we studied the phylogeographical structure of the red-necked snow finch Pyrgilauda ruficollis, an endemic species of the Tibetan plateau. We analysed 879 base pairs (bp) of the mitochondrial cytochrome b gene and 529 bp of the control region in 41 birds from four regional groups separated by mountain ranges. We detected 34 haplotypes, 31 of which occurred in a single individual and only three of which were shared among sampling sites within regional groups or among regional groups. Haplotype diversity was high (h = 0.94); nucleotide diversity was low (ð = 0.00415) and genetic differentiation was virtually non-existent. Analyses of mismatch distributions and geographically nested clades yielded results consistent with contiguous range expansion, and the expansion times were estimated as 0.07,0.19 million years ago (Ma). Our results suggest that P. ruficollis colonized the Tibetan plateau after the extensive glacial period (0.5,0.175 Ma), expanding from the eastern margin towards the inner plateau. Thus, in contrast to many of the postglacial phylogeographical structures known at high latitudes, this colonization occurred without matrilineal population structuring. This might be due to the short glacial cycles typical of the Tibetan plateau, adaptation of P. ruficollis to cold conditions, or refugia and colonized habitat being semicontinuous and thus promoting population mixing. [source]

Patterns of permafrost formation and degradation in relation to climate and ecosystems

PERMAFROST AND PERIGLACIAL PROCESSES, Issue 1 2007
Y. L. Shur
Abstract We develop a permafrost classification system to describe the complex interaction of climatic and ecological processes in permafrost formation and degradation that differentiates five patterns of formation: ,climate-driven'; ,climate-driven, ecosystem-modified'; ,climate-driven, ecosystem-protected'; ,ecosystem-driven'; and ,ecosystem-protected' permafrost. Climate-driven permafrost develops in the continuous permafrost zone, where permafrost forms immediately after the surface is exposed to the atmosphere and even under shallow water. Climate-driven, ecosystem-modified permafrost occurs in the continuous permafrost zone when vegetation succession and organic-matter accumulation lead to development of an ice-rich layer at the top of the permafrost. During warming climates, permafrost that has formed as climate-driven can occur in the discontinuous permafrost zone, where it can persist for a long time as ecosystem-protected. Climate-driven, ecosystem protected permafrost, and its associated ground ice, cannot re-establish in the discontinuous zone once degraded, although the near surface can recover as ecosystem-driven permafrost. Ecosystem-driven permafrost forms in the discontinuous permafrost zone in poorly drained, low-lying and north-facing landscape conditions, and under strong ecosystem influence. Finally, ecosystem-protected permafrost persists as sporadic patches under warmer climates, but cannot be re-established after disturbance. These distinctions are important because the various types react differently to climate change and surface disturbances. For example, climate-driven, ecosystem-modified permafrost can experience thermokarst even under cold conditions because of its ice-rich layer formed during ecosystem development, and ecosystem-driven permafrost is unlikely to recover after disturbance, such as fire, if there is sufficient climate warming. Copyright © 2007 John Wiley & Sons, Ltd. [source]

Neandertal cold adaptation: Physiological and energetic factors

AMERICAN JOURNAL OF HUMAN BIOLOGY, Issue 5 2002
A. Theodore Steegmann Jr.
European Neandertals employed a complex set of physiological cold defenses, homologous to those seen in contemporary humans and nonhuman primates. While Neandertal morphological patterns, such as foreshortened extremities and low relative surface-area, may have explained some of the variance in cold resistance, it is suggested the adaptive package was strongly dependent on a rich array of physiological defenses. A summary of the environmental cold conditions in which the Neandertals lived is presented, and a comparative ethnographic model from Tierra del Fuego is used. Muscle and subcutaneous fat are excellent "passive" insulators. Neandertals were quite muscular, but it is unlikely that they could maintain enough superficial body fat to offer much cold protection. A major, high-energy metabolic adaptation facilitated by modest amounts of highly thermogenic brown adipose tissue (BAT) is proposed. In addition, Neandertals would have been protected by general mammalian cold defenses based on systemic vasoconstriction and intensified by acclimatization, aerobic fitness, and localized cold-induced vasodilation. However, these defenses are energetically expensive. Based on contemporary data from circumpolar peoples, it is estimated that Neandertals required 3,360 to 4,480 kcal per day to support strenuous winter foraging and cold resistance costs. Several specific genetic cold adaptations are also proposed,heat shock protein (actually, stress shock protein), an ACP*1 locus somatic growth factor, and a specialized calcium metabolism not as yet understood. Am. J. Hum. Biol. 14:566,583, 2002. © 2002 Wiley-Liss, Inc. [source]

GIGANTEA is a component of a regulatory pathway determining wall ingrowth deposition in phloem parenchyma transfer cells of Arabidopsis thaliana

THE PLANT JOURNAL, Issue 4 2010
Joshua Edwards
Summary Transfer cells are specialised transport cells containing invaginated wall ingrowths that generate an amplified plasma membrane surface area with high densities of transporter proteins. They trans -differentiate from differentiated cells at sites at which enhanced rates of nutrient transport occur across apo/symplasmic boundaries. Despite their physiological importance, little is known of the molecular mechanisms regulating construction of their intricate wall ingrowths. We investigated the genetic control of wall ingrowth formation in phloem parenchyma transfer cells of leaf minor veins in Arabidopsis thaliana. Wall ingrowth development in these cells is substantially enhanced upon exposing plants to high-light or cold treatments. A hierarchical bioinformatic analysis of public microarray datasets derived from the leaves of plants subjected to these treatments identified GIGANTEA (GI) as one of 46 genes that are commonly up-regulated twofold or more under both high-light and cold conditions. Histological analysis of the GI mutants gi-2 and gi-3 showed that the amount of phloem parenchyma containing wall ingrowths was reduced 15-fold compared with wild-type. Discrete papillate wall ingrowths were formed in gi-2 plants but failed to develop into branched networks. Wall ingrowth development in gi-2 was not rescued by exposing these plants to high-light or cold conditions. In contrast, over-expression of GI in the gi-2 background restored wall ingrowth deposition to wild-type levels. These results indicate that GI regulates the ongoing development of wall ingrowth networks at a point downstream of inputs from environmental signals. [source]

A Holocene lacustrine record of environmental change in northeastern Prince of Wales Island, Nunavut, Canada

BOREAS, Issue 4 2001
KONRAD GAJEWSKI
A core from Prince of Wales Island in the central Canadian Arctic was analysed for pollen and sediment characteristics. From 9200 yr BP to 7000 yr BP, the landscape supported a pioneer vegetation under cold conditions, with relatively high sediment input to the lake. Between 7000 and 4000 yr BP there was a period of high pollen concentrations, more abundant Cyperaceae and Dryas on the landscape and finer sediment input. In the last 4000 years, climate cooling is indicated. [source]