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51.
Summary The Linnaean nameCryptozo?n proliferum
Hall was proposed in 1883 for a previously undescribed life-form preserved in spectacular exposures of Cambrian limestones in
New York State, USA. It is now recognised that these are exposures of stromatolitic microbialites, laminated organosedimentary
structures formed from interaction between a benthic microbial community (BMC) and the environment. Microbialites are neither
fossil organisms nor trace fossils. These complex structures are the products of dissipative, self-organising systems involving
a BMC, the external environment and the accreting microbialite. Functionally analogous BMCs of different species compositions
may build similar structures in similar environments in quite separate periods. The type exposures ofCryptozo?n proliferum show objects composed of complex, concentric rings, up to a metre in diameter, that have grown laterally without any restriction
other than that provided by neighbouring structures. They are not the relicts of domes truncated by penecontemporaneous erosion
or Pleistocene glaciation, but depositional forms in which upward growth was restricted. Analogous modern structures occur
on a reef platform along the north east shore of hyposaline Lake Clifton, Western Australia. These are tabular thrombolitic
microbialites that vary lakeward across the reef platform from low, compound structures to discrete, concentric structures
up to 50 cm high. The Lake Clifton forms are, in turn, morphological analogues of microatolls found on coral reef platforms.
Coral microatolls are coral colonies with flat, dead tops and living perimeters in which upward growth is constrained by the
sea surface. In shallow water they form circular rims of laterally growing coral around a dead centre. In deeper water they
form coral heads that develop flat tops on reaching sea level. It is concluded that both the tabular microbialites of Lake
Clifton and the type exposures ofCryptozo?n proliferum are analogous to coral microatolls in both form and origin-structures that have been able to grow laterally, but in which
upward growth is restricted by subaerial exposure. Similar microatoll microbialites have been described from other modern
environments, including Great Salt Lake, Utah, USA and Stocking Island, Exuma Cays, Bahamas. Ancient examples may include
some of the “tufa” deposits of the Basal Purbeck Formation in Dorset, UK, as well as the coalesced domal bioherms of the Upper
Cambrian Arrinthrunga Formation of the Georgina Basin, Central Australia, and the “washbowl” structures described from the
B?tsfjord Formation of the Varanger Peninsula, north Norway. Progress towards a reliable interpretation of ancient microbialites
depends on an understanding of modern environments in which analogous structures are forming. This study of microatolls has
demonstrated that other sessile life forms may create colonial ecomorphs that, used cautiously, can serve as analogues for
understanding the factors controlling the growth and form of microbialites. The surprising lack of pre-Pleistocene examples
of microatolls recorded to date has simply been due to their lack of recognition in the geological record. They occur in sequences
from the Proterozoic onwards, and provide powerful environmental indicators of ancient reef platforms on which biological
growth was adjusted to contemporary sea level. 相似文献
52.
杭州西湖水质预测方法和结果分析 总被引:1,自引:0,他引:1
本文利用二维对流扩散模型对西湖水质总磷浓度进行预测,给出方程的理论基础,编制FORTRAN77程序,在386微机上实现预测,并对预测结果作了较为详细的分析.本模型对水质环境防治决策具有实际意义. 相似文献
53.
Conservation of salt lakes 总被引:2,自引:2,他引:0
W. D. Williams 《Hydrobiologia》1993,267(1-3):291-306
Salt lakes have a variety of important uses and values, including especially both economic and scientific ones. These uses and values have been and are increasingly subject to degradation from a variety of impacts: diversion of inflows, pollution, agricultural practices, and introduction of exotic species are among the more important. Recognition of these impacts upon salt lakes has led to some international and national measures for their conservation, but considerably more effort in this direction is needed. Against this background, Mono Lake, California, USA, and the Aral Sea, central Asia, are discussed as two localities which bring into sharp focus the various matters discussed in the paper. Finally, attention is drawn to the need to conserve the Akrotiri Salt Lake, Cyprus. 相似文献
54.
The densities of alkali fly larvae and pupae were measured in relation to depth and substrate type at six locations around Mono Lake. Samples representing a mixture of different bottom features were taken to a depth of 10 m (33 ft) using SCUBA. This is at or near the depth limit of fly larvae and pupae. The biomass of larvae and pupae on hard substrate were maximum and approximately equal at depths of 0.5 m and 1 m, substantially lower at intermediate depths of 3 m and 5 m, and over an order of magnitude further reduced at 10 m. Densities of flies on hard or rocky substrates (mainly calcareous tufa deposits), were significantly greater than those found on soft substrates such as mud or sand, at all but the greatest depth surveyed.Bathymetric maps of the areas of hard and soft substrate occurring at different lake depths were used to estimate the fly population size over the whole lake, based on the density distribution of larvae and pupae with depth on different substrates. The mapped areas of soft and hard substrates were also calculated for different lake levels, and applying the same procedure, a population model comparing the abundance of flies at different lake levels was developed. This habitat-based population model predicts that the abundance of the alkali fly is maximized at 6380 ft (1945 m) lake surface elevation. Most of the tufa substrate submerged at this lake level will become exposed and unavailable as habitat as the lake declines to 6370 ft (1942 m). In late 1991, the lake level was just over 6374 ft (1943 + m). 相似文献
55.
Climate change has profound effects on forest ecosystems. Schrenk spruce (P. schrenkiana) is a natural conifer species endemic to the arid inland areas of Asia. In this study, the relationship between tree-ring parameters of P. schrenkiana and major meteorological factors were analyzed, and the main limiting factors for tree radial growth and stable carbon isotope fractionation were explored. Our results indicate that moisture stress before and during the growing season have an important influence on radial growth of P. schrenkiana, especially, the correlation coefficient between tree-ring width and vapor pressure deficit (VPD) from previous August to current July is as high as −0.622 (n = 51, p < 0.01). Collinearity analysis further supports the conclusion that the limiting factor for the radial growth of P. schrenkiana is moisture. Although the correlation analysis results show that the tree-ring δ13Ccorr is significantly positively correlated with sunshine duration (SD), additional analysis based on first order difference variables suggests that the climate factor may not be the only limiting factor for the stable carbon isotope fractionation of tree rings in the Sayram Lake Basin. This lays the foundation for the assessment of forest management practices and carbon sink capacity in light of future climate change. 相似文献
56.
As one of the basic theories of biodiversity conservation, island biogeography has been widely accepted in the past
decades. Originally, island biogeography was put forward and applied in oceanic environments. But later on, it
was found out that the application was not only limited to oceanic islands, but also in terrestrial environments
with relatively isolated conditions. In terms of biodiversity level, island biogeography generally focuses on a small
scale, such as species diversity and genetic diversity. The studies of biodiversity on a large-scale based on island
biogeography, such as ecosystem and landscape scales, were seldomly conducted. Taking Poyang Lake, the largest
fresh water lake in China as case study area, 30 grasslands were randomly selected to study whether island biogeography can be applied to grasslands at a landscape level from three island attributes (area, distance and shape),
and the most important ecological variable (flooding) in Poyang Lake. The results showed that in general, grasslands have the property of an island, and follow the basic principle of island biogeography. We found the area and
flooding duration were the two most important determinants of landscape diversity. There was a significant positive correlation between the grassland area and the landscape diversity, which could be well expressed by logarithmic function model (R2 = 0.73). There was a negative correlation between flooding duration and landscape
diversity, which could be described by an inverse model (R2 = 0.206). The distance to mainland and the shape
of grassland were correlated with landscape diversity, but the fitting result of the models was not as good as
expected. The possible reason could be that Poyang Lake is a seasonal lake, the water level varies with hydrological
conditions, so that the grasslands are not strongly isolated and their shape is not stable enough required by island
biogeography. Furthermore, it indicates that besides area, distance and shape attributes, flooding strongly affects
the biodiversity of grassland vegetation, and should not be ignored when applying island biogeography theory to
Poyang Lake. This study is expected to be a supplement for island biogeography in terrestrial environments, and
the results are expected to benefit for the biodiversity conservation in Poyang Lake. 相似文献
57.
Manfred Rösch 《Vegetation History and Archaeobotany》1993,2(4):213-232
The second part of a pollen profile from Hornstaad/Lake Constance (Germany), containing the Atlantic and Subboreal (6400 cal B.C. to 700 cal B.C.) is presented. The diagram has a sampling interval of 1 cm and an average time resolution of 10 years. The cereal curve provided the basis for cereal zones, which are used to classify the human impact. Twenty-six cereal zones can be distinguished, most of them divided into subzones, from 5500 cal B.C. to 700 cal B.C. They correspond to both known and, mostly, unknown settlements in the surrounding landscape from the Early Neolithic to the Late Bronze Age. Charcoal and chemical analyses as well as sediment accumulation, confirmed by accelerator dates, provide evidence for human impact on the environment.A contribution to the 8th IPC, Aix-en-Provence, Sept. 1992 相似文献
58.
Enrichment cultures of littoral benthic algae from Mono Lake, California, and Abert Lake, Oregon, were grown under conditions of varied salinity and nutrient content. Field-collected inocula were composed mainly of diatoms and filamentous blue-green and green algae. The yield of long-term cultures (30 days) showed tolerance over a broad salinity range (50–150 g·L?1) for Mono Lake-derived algae. Algae from Abert Lake had a lower range of tolerance (25–100 g·L?1) Organic content and pigment concentrations of algae from both lakes were also reduced above the tolerated salinity level. Within the range of salinity tolerance for Mono Lake algae, initial growth rates and organic content were reduced by increased salinity. The effects of macro- and micronutrient enrichment on algal growth in Mono Lake water were also tested. Only nitrogen enrichment (either as ammonium or nitrate) stimulated algal growth. Although the benthic algae cultured here had wide optima for salinity tolerance, the rates of growth and storage were limited by increased salinity within the optimum range. Although the lakes compared had similar species composition, the range and limits of tolerance of the algae were related to salinity of the lake of origin. 相似文献
59.
Astrid Löffler Justyna Wolinska Barbara Keller Karl-Otto Rothhaupt Piet Spaak 《Freshwater Biology》2004,49(10):1372-1380
1. We investigated whether Daphnia galeata × hyalina hybrids of Lake Constance and Lake Greifensee show the same pattern of life history parameters as previously reported for D. galeata × cucullata hybrids and whether such a pattern is consistent between Daphnia populations from those two lakes. 2. Hybrids in Lake Constance were intermediate in size compared with the parental species. Hybrids in Lake Greifensee were smaller than D. galeata. The intrinsic growth rate (r) of hybrids from Lake Constance was not significantly different from the faster growing parental taxon D. galeata. However, r of hybrids from Lake Greifensee was significantly lower than that of D. galeata. 3. The observed juvenile body length differences between the taxa varied with the clutch number. The first clutch juvenile lengths of the three taxa did not differ for Lake Constance. First clutch juveniles of Lake Greifensee D. galeata were smaller than hybrid first clutch juveniles. The third clutch juvenile length did not differ between taxa from Lake Greifensee, but D. galeata juveniles from Lake Constance were bigger than those of D. hyalina. 4. The life history pattern found in Lake Constance corresponds to previous findings from other studies. The hybrids in this lake combine the faster population growth of one parental species with a relatively small size. In the case of Lake Greifensee hybrids, the relatively large size of first clutch juveniles and the small size of the adults could be interpreted as dual adaptations to invertebrate and fish predation. We speculate that the lower population growth rate of the hybrids is a trade‐off for this twofold protection. 相似文献
60.