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At least 811 records · Page 45Linked to original sources
PubMed2005

Impacts of orbital forcing and atmospheric carbon dioxide on Miocene ice-sheet expansion.

The processes causing the middle Miocene global cooling, which marked the Earth's final transition into an 'icehouse' climate about 13.9 million years ago (Myr ago), remain enigmatic. Tectonically driven circulation changes and variations in atmospheric carbon dioxide levels have been suggested as driving mechanisms, but the lack of adequately preserved sedimentary successions has made rigorous testing of these hypotheses difficult. Here we present high-resolution climate proxy records, covering the period from 14.7 to 12.7 million years ago, from two complete sediment cores from the northwest and southeast subtropical Pacific Ocean. Using new chronologies through the correlation to the latest orbital model, we find relatively constant, low summer insolation over Antarctica coincident with declining atmospheric carbon dioxide levels at the time of Antarctic ice-sheet expansion and global cooling, suggesting a causal link. We surmise that the thermal isolation of Antarctica played a role in providing sustained long-term climatic boundary conditions propitious for ice-sheet formation. Our data document that Antarctic glaciation was rapid, taking place within two obliquity cycles, and coincided with a striking transition from obliquity to eccentricity as the drivers of climatic change.

Antarctic Regions↗
PubMed2005

The Arabidopsis cold-responsive transcriptome and its regulation by ICE1.

To understand the gene network controlling tolerance to cold stress, we performed an Arabidopsis thaliana genome transcript expression profile using Affymetrix GeneChips that contain approximately 24,000 genes. We statistically determined 939 cold-regulated genes with 655 upregulated and 284 downregulated. A large number of early cold-responsive genes encode transcription factors that likely control late-responsive genes, suggesting a multitude of transcriptional cascades. In addition, many genes involved in chromatin level and posttranscriptional regulation were also cold regulated, suggesting their involvement in cold-responsive gene regulation. A number of genes important for the biosynthesis or signaling of plant hormones, such as abscisic acid, gibberellic acid, and auxin, are regulated by cold stress, which is of potential importance in coordinating cold tolerance with growth and development. We compared the cold-responsive transcriptomes of the wild type and inducer of CBF expression 1 (ice1), a mutant defective in an upstream transcription factor required for chilling and freezing tolerance. The transcript levels of many cold-responsive genes were altered in the ice1 mutant not only during cold stress but also before cold treatments. Our study provides a global picture of the Arabidopsis cold-responsive transcriptome and its control by ICE1 and will be valuable for understanding gene regulation under cold stress and the molecular mechanisms of cold tolerance.

Adaptation, Physiological↗
PubMed1988

[Ecological characteristics of the structural organization of respiratory segments of the lung].

The structure of the bronchial tree in the lung lobules has been studied and the number of lobules and acini in different lobes and in the entire lung has been determined in polar foxes and dogs. Branching pattern and the number of generations of interlobular and intralobular bronchioli have been defined. It has been found that the number of lung lobules in polar foxes was twice as high as in dogs, the lobule volume being smaller almost by half. A smaller number of acini in polar fox lobules enables the central regulation mechanisms to intensify the control of local ventilation. It broadens the possibilities for physiological responses to the influence of climatic factors of the Extreme North.

Animals↗
PubMed2002

Winter water relations of New England conifers and factors influencing their upper elevational limits. II. Modeling.

We used the water relations model, WINWAT, to model winter water relations of three conifer species-eastern hemlock (Tsuga canadensis (L.) Carr.), eastern white pine (Pinus strobus L.) and red pine (P. resinosa Ait.)-growing at their upper elevational limits on Mt. Ascutney, Vermont, USA, in the winters of 1997 and 1999. Modeled relative water contents remained above 60% in the two youngest foliar age classes of all three species during both winters, indicating that desiccation stress in winter is not responsible for setting the upper elevational limits of these species at this site under present climatic conditions. WINWAT indicated that winter water relations of these low-elevational species were sensitive to low relative humidity, which increased transpiration rates, and low temperatures, which inhibited recharge, but are much less sensitive to summer climate than in the case of subalpine conifers in Colorado. Our results indicate that summer and winter temperatures and relative humidities (or precipitation/potential evapotranspiration ratios) should be incorporated into climate change models designed to simulate future tree distributions.

Altitude↗
PubMed1988

[Chronic alcoholic enteritis in the North].

Altogether 107 patients with chronic enterocolitis were examined. They were divided into 3 groups with relation to their attitude to alcohol: the 1st group-alcoholics, the 2nd risk group-hard drinking, the 3rd group-non-alcoholics. Severe disorders of the intestinal enzymatic activity (suppression of the intraduodenal amylolytic and proteolytic and intraluminal lactase activity) were revealed, the character of parietal digestion was changed. Atrophic duodenal changes among these patients were noted twice as more frequently as among the patients who did not consume alcohol or consumed it moderately. Expeditions revealed positive correlation between the morbidity and the type of living conditions in one or another climatic geographic area in the Jakut Republic.

Adult↗
PubMed1985

Sexual activity of Holstein cows: seasonal effects.

Continuous observations of Holstein dairy cows during natural and prostaglandin-induced estrus were conducted to determine effects of cold and hot weather on the degree and pattern of sexual activities, circadian profile of activities, and location of activities. Mounts with pelvic thrusts and mounts plus 12 other estrous-related activities for 73 cows were monitored for 96 h in cold weather and 120 h in hot weather. Eleven cows in hot weather with more than one mount were in estrus longer with less intensity of mounting than 16 cows in cold weather; climate did not affect mounts received or total activities initiated per cow. Number of cows in standing estrus affected mounts received per cow, total activities received per cow, and time in estrus but not activities initiated per animal. Two estrual cows in cold weather and 6 cows in hot weather received less than 2 mounts. Cows in cold weather had more (28%) total estrous activity as mounting activity than cows in hot weather (14%); cows in hot weather interacted more by rubbing and licking than cows in cold weather. Cows in cold weather had more mounting activity from 0600 to 1759 h (73%) than from 1800 to 0559 h (27%) and had more mounts from 1200 to 1759 h than cows in hot weather. During both cold and hot weather, sexual activities decreased at milking time. In the freestall housing with drylot, 80% of the mounting activity in both climates occurred in an outdoor drylot and feed manger area, which had best footing. These data indicate that climate affected mounting and total sexual activity of lactating dairy cows.

Animals↗
PubMed2003

Sea-level fluctuations during the last glacial cycle.

The last glacial cycle was characterized by substantial millennial-scale climate fluctuations, but the extent of any associated changes in global sea level (or, equivalently, ice volume) remains elusive. Highstands of sea level can be reconstructed from dated fossil coral reef terraces, and these data are complemented by a compilation of global sea-level estimates based on deep-sea oxygen isotope ratios at millennial-scale resolution or higher. Records based on oxygen isotopes, however, contain uncertainties in the range of +/-30 m, or +/-1 degrees C in deep sea temperature. Here we analyse oxygen isotope records from Red Sea sediment cores to reconstruct the history of water residence times in the Red Sea. We then use a hydraulic model of the water exchange between the Red Sea and the world ocean to derive the sill depth-and hence global sea level-over the past 470,000 years (470 kyr). Our reconstruction is accurate to within +/-12 m, and gives a centennial-scale resolution from 70 to 25 kyr before present. We find that sea-level changes of up to 35 m, at rates of up to 2 cm yr(-1), occurred, coincident with abrupt changes in climate.

Animals↗
PubMed2004

Regional climate shifts caused by gradual global cooling in the Pliocene epoch.

The Earth's climate has undergone a global transition over the past four million years, from warm conditions with global surface temperatures about 3 degrees C warmer than today, smaller ice sheets and higher sea levels to the current cooler conditions. Tectonic changes and their influence on ocean heat transport have been suggested as forcing factors for that transition, including the onset of significant Northern Hemisphere glaciation approximately 2.75 million years ago, but the ultimate causes for the climatic changes are still under debate. Here we compare climate records from high latitudes, subtropical regions and the tropics, indicating that the onset of large glacial/interglacial cycles did not coincide with a specific climate reorganization event at lower latitudes. The regional differences in the timing of cooling imply that global cooling was a gradual process, rather than the response to a single threshold or episodic event as previously suggested. We also find that high-latitude climate sensitivity to variations in solar heating increased gradually, culminating after cool tropical and subtropical upwelling conditions were established two million years ago. Our results suggest that mean low-latitude climate conditions can significantly influence global climate feedbacks.

Animals↗
PubMed2002

[The functional morphology of polytene chromosomes in the midge Chironomus pilicornis F. from the permafrost zone reservoirs].

The karyotype and chromosomal polymorphism of Chironomus pilicornis from the reservoirs of Yakutian permafrost zone are described. In the Yakutian populations, of 10 inversion sequences 11 genotypical combinations of these were registered. The level of inversion heterozygosity is 50-70%, but in several populations it makes only 11-29%. In comparison with the Scandinavian populations, significant functional modifications of chromosomal morphology were found. They are associated with the increase in centromeric heterochromatin amount, facultative chromocentre formation, and the appearance of numerous B-chromosomes and nucleoli, including the facultative ones. A possible adaptive significance of such functional modifications conditioned by climate peculiarities is discussed.

Adaptation, Biological↗
PubMed1976

[Meteorotropy of vasomotor cephalea].

During a period of 823 days (from 1st October 1971 to 31st December 1973), attacks of migraine, non-migraine vascular cephalea and cephalea due to other neighbouring disturbances strong enough to affect working capacity were studied in 4 subjects. 2152 pieces of data were collected. 2) Frequency was at a minimum in summer and peaked in spring and autumn. 3) Comparison with meteorological conditions points to a highly significant recrudescence of disturbances in cold, damp weather, and meteorological periodicity independent of biological (circadian) rhythms.

Adaptation, Physiological↗
PubMed2002

On-line analysis of urban particulate matter focusing on elevated wintertime aerosol concentrations.

A 10-day winter sampling campaign was conducted in downtown Toronto for particulate matter (PM) air pollution in the fine (<2.5 microm) size range. An aerosol laser ablation mass spectrometer (LAMS), a tapered-element oscillating microbalance (TEOM), and an aerodynamic particle sizer (APS) were operated in parallel to characterize the PM on-line. In this study, the LAMS observed differences in the chemical composition between three separate episodes with higher PM2.5 mass and APS counts. LAMS results showed that in one instance of elevated PM, organic amines were present in the particulates. Temporal analyses of this episode revealed chemical transformations as the amines, characterized by m/z peaks 58(C3HeN)+, 86(C5H2N)+, and nitrates, increased in number concentration while Ca and hydrocarbon particle classes concurrently decreased. On another day, sulfates were found to have increased significantly. The third event was only 4 h in duration and exhibited an increase in the number of submicron-sized K/hydrocarbons and sulfate-containing particles. In this last event, the hydrocarbons and a K to Fe ratio enrichment indicated there was likely a contribution from a combustion source. This work offers some of the first insights into single particle size and chemistry in a cold winter climate.

Aerosols↗