Classification and ordination of the alpine plant communities of Railroad Ridge, White Cloud Peaks, Idaho

Alpine vegetation of Railroad Ridge in the White Cloud Peaks, Custer County, Idaho, was investigated to ascertain native communities and describe their distribution with respect to important environmental factors. Percent cover of all species and environmental information were recorded for 69 plots. Data were analyzed by TWINSPAN and CANOCO, which provided a classification and an ordination, respectively. Predominant communities are dominated by (1) Phlox pulvinata , (2) Carex elynoides , and (3) Ceum rossii , and other communities of lesser importance are dominated by (4) Artemisia campestris , (5) Eriogonum ovalifolium and Silene acaulis , and (6) Ivesia gordonii . Although the Artemisia campestris community occupies a relatively small portion of the study area, it is noteworthy because it is a community type not previously known for Idaho. The community co-dominated by Eriogonum ovalifolium and Silene acaulis is also unique and has not been documented in other Idaho alpine studies. Community distribution showed the strongest correlation with exposure, substrate type, and slope. In general, the study area supports fellfield communities that are representative of alpine areas in Idaho and some Great Basin mountain ranges, and dense turflike communities similar to ones found throughout western North America's temperate alpine regions.     

Some aspects of succession in the spruce-fir forest zone of northern Utah

A site in the Rocky Mountain subalpine forest zone with which a series of hypotheses concerning ecosystem succession was tested is characterized. Succession from herb-dominated meadows to climax forests of Engelmann spruce and subalpine fir can follow at least four identified pathways. After fire, spruce and fir may reinvade a site directly, follow invasion by aspen, or follow invasion by lodgepole pine, the pathway depending on a combination of physical and biotic factors. In other cases, succession begins with long-established meadows which do not owe their existence to fire. In this latter pathway, aspen invades meadows by suckering and changes the environment near the soil surface so as to facilitate establishment of the climax tree species. The biota and soils of four characteristic seral stages (meadow, aspen, fir, spruce-fir) in this latter pathway are described.     

Captopril (SQ 14225) depresses drinking and aldosterone in rats lacking vasopressin.

Angiotensin II is dipsogenic, and vasopressin (ADH) regulates renal water excretion. Together, these hormones govern overall mammalian water balance. The Brattleboro rat with inherited diabetes insipidus (DI) lacks ADH and is therefore a convenient model with which to elucidate mechanisms regulating water metabolism. In the present studies, angiotensin II has also been removed from DI rats by the administration of an inhibitor (captopril, SQ 14225; D-2-methyl-3-mercaptopropanoyl-L-proline) of the enzyme which converts angiotensin I, the relatively inert component of the renin-angiotensin system, to angiotensin II, the biologically active substance. SQ 14225 reduced the drinking rates, and after 6 days lowered peripheral plasma aldosterone concentrations were associated with hyperkalaemia. We conclude that the polydipsia of diabetes insipidus partly results from elevated plasma renin activities and angiotensin II concentrations seen in this syndrome. Further, the apparent hypoaldosteronism of DI Brattleboro rats reflects differences in both tissue usage of the steroid and adrenocortical sensitivities associated with polyuria, hyperosmolarity and possibly potassium wasting.     

Ice-sheet collapse and sea-level rise at the Bølling warming 14,600 years ago

Past sea-level records provide invaluable information about the response of ice sheets to climate forcing. Some such records suggest that the last deglaciation was punctuated by a dramatic period of sea-level rise, of about 20?metres, in less than 500?years. Controversy about the amplitude and timing of this meltwater pulse (MWP-1A) has, however, led to uncertainty about the source of the melt water and its temporal and causal relationships with the abrupt climate changes of the deglaciation. Here we show that MWP-1A started no earlier than 14,650 years ago and ended before 14,310 years ago, making it coeval with the B?lling warming. Our results, based on corals drilled offshore from Tahiti during Integrated Ocean Drilling Project Expedition 310, reveal that the increase in sea level at Tahiti was between 12 and 22 metres, with a most probable value between 14 and 18 metres, establishing a significant meltwater contribution from the Southern Hemisphere. This implies that the rate of eustatic sea-level rise exceeded 40 millimetres per year during MWP-1A.     

A carbon- and oxygen-isotope record of recent environ- mental change from Qinghai Lake, NE Tibetan Plateau

An understanding of natural climatic variability is essential for evaluating anthropogenic impacts on recent and future climate[1—3]. Due to the lack of lengthy instrumental records, such an understanding must be gained from natural archives of climate change. Palaeolimnological indicators of past lake levels may provide a sensitive record of changes in effective precipitation in closed basins. This approach is particularly relevant on the Tibetan Plateau, where instrumental records are very…     

Nucleolus organizer region location and ‘ring’ chromosomes in the bharal

Summary Silver-staining has been used to identify the nucleolus organizer regions (NORs) in the bharal. These show homology with sheep, goat, cattle and aoudad. The association of the NORs on both telomeres of chromosome 3 results in a ring chromosome.     

Assessing the impact of population stratification on genetic association studies

Population stratification refers to differences in allele frequencies between cases and controls due to systematic differences in ancestry rather than association of genes with disease. It has been proposed that false positive associations due to stratification can be controlled by genotyping a few dozen unlinked genetic markers. To assess stratification empirically, we analyzed data from 11 case-control and case-cohort association studies. We did not detect statistically significant evidence for stratification but did observe that assessments based on a few dozen markers lack power to rule out moderate levels of stratification that could cause false positive associations in studies designed to detect modest genetic risk factors. After increasing the number of markers and samples in a case-cohort study (the design most immune to stratification), we found that stratification was in fact present. Our results suggest that modest amounts of stratification can exist even in well designed studies.