• Volume 30,Issue 1,2010 Table of Contents
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    • New judgement on the source of soil water in extremely dry zone

      2010, 30(1):1-7. DOI: 10.1016/j.chnaes.2009.12.001

      Abstract (243) HTML (0) PDF 895.17 K (282) Comment (0) Favorites

      Abstract:There is always a relatively high moisture content in the shallow soil layer in Gobi area on the top of the Mogao Grottoes in the extremely dry zone. This paper gives out a new judgement on soil water source through field experiments using the isolated water method, simulated rainfall method and greenhouse method. Under the condition of typical hyper-arid climate far away from rainfall effect and after cutting off the connection of soil and groundwater the simulated rainfall experiment was conducted, through putting up a plastic greenhouse to obtain a relatively closed space and extracting the condensed water on the film surface, the soil water output from the greenhouse was monitored. The experimental results show that generally the rainfall can be completely evaporated in about 20 days under the isolated condition. In the relatively closed space sheltered by arched greenhouse in the Gobi area water can be continuously transferred outward from subsoil and condensed on the roof film, with a daily output quantity of 3–5 g/m2d. After prolonged output soil water content remains significantly higher than that of the control and before covering by arched shed. Comprehensively judging from this, groundwater is an important source of soil water in addition to precipitation. The new judgement has a very important practical significance to the water research of the groundwater–soil–plant-atmosphere circle (GSPAC) and the recovery of the desertified environment.

    • Advance in the toxic effects of petroleum water accommodated fraction on marine plankton

      2010, 30(1):8-15. DOI: 10.1016/j.chnaes.2009.12.002

      Abstract (540) HTML (0) PDF 202.67 K (1841) Comment (0) Favorites

      Abstract:Recently, the impact of petroleum pollution on marine plankton has been complemented by a great concern. This review summarizes the reports about toxic effects of oil water accommodated fraction (WAF) on marine phytoplankton, zooplankton and early life stage of animal. For the oil WAF, toxicants are mainly composed of the aromatic hydrocarbons, such as the benzene hydrocarbons and polycyclic aromatic hydrocarbons (PAHs) with 2–5 rings. The oil WAF, especially the PAHs, can be accumulated in plankton due to their great lipophilic abilities, and thus elicites various deleterious effects. Toxicological tests show that marine plankton is very sensitive to the petroleum WAF, as the order of median effective/lethal concentration is merely μg/L or mg/L. There are species and developmental stages differences of plankton tolerance to petroleum WAF, and the toxicity of different oil WAF is various. Generally, its toxicity enhances with increasing carbonic chain length and benzene ring number. Many studies on the acute and sub-acute toxic effects of oil WAF have been done, however few researches on its chronic toxic effects has been carried out till now. Besides, most reports focused on the levels from molecule to individual, though very little work of petroleum toxic effects has ever been performed on the marine plankton population or community levels. Therefore, it is necessary to continue these studies in future.

    • Effects of water depth and substrate type on growth dynamics and biomass allocation of Oryza rufipogon

      2010, 30(1):16-21. DOI: 10.1016/j.chnaes.2009.12.003

      Abstract (114) HTML (0) PDF 380.10 K (7) Comment (0) Favorites

      Abstract:Oryza rufipogon is known as the ancestor of Asian cultivated rice (Oryza sativa) and the most important germplasm for rice improvement. In this study, we investigated its growth and biomass allocation in response to water depth and substrate type. The results demonstrated that individual plant had an average weight of 18.98 g, 9.36 g, and 10.59 g and produced 77.7 seeds, 35.5 seeds, and 41.6 seeds in deep-, fluctuated-, and shallow water, respectively. Root-to-shoot ratios were 0.37 in deep water, 0.61 in fluctuated water level, and 0.56 in shallow water, reflecting larger investment in roots under water-level fluctuation and shallow water conditions. However, biomass allocation for sexual reproduction was no significant different among the three water levels. In substrates experiment, total biomass and seed production were significantly different between sediment types, and the averages were 10.59 g, 3.56 g, and 0.76 g in biomass and 41.6 seeds, 13.8 seeds, and 0.5 seeds per plant in lake sediment, river sand and clay, respectively. The number of tillers was significantly fewer in sandy and clay substrates than in lake sediments. Individual plant in clay substrates was significantly shorter than those in sandy and in lake sediment substrates. Our study suggests that the plasticity in morphology and biomass allocation of O.rufipogon appears to be an adaptation to the variability in water level and substrate conditions.

    • Feeding efficiency of a marine copepod Acartia erythraea on eight different algal diets

      2010, 30(1):22-26. DOI: 10.1016/j.chnaes.2009.12.004

      Abstract (243) HTML (0) PDF 242.16 K (11) Comment (0) Favorites

      Abstract:Acartia erythraea is a dominant zooplankton copepod in the South China coastal waters during summer. This paper examined its feeding behavior (food gut passage, clearance rate and ingestion rate) on eight phytoplankton diets. The food gut passage time and ingestion rate were negatively related to the size and concentration of food supply, whereas the clearance rate was positively related to the food concentration. The ingestion rate decreased with the food concentration when it reached a threshold level. Generally, the clearance rate of copepods decreased with increasing cell density, but was very low at both low and high algal densities when the food were small in sizes. The optimum food size was about 10 μm for the copepods, and the dinoflagellate, Prorocentrum minimum, was considered as a good food choice for A. erythraea.

    • Landscape patterns and their changes in Sichuan Ruoergai Wetland National Nature Reserve

      2010, 30(1):27-32. DOI: 10.1016/j.chnaes.2009.12.005

      Abstract (665) HTML (0) PDF 448.14 K (391) Comment (0) Favorites

      Abstract:In Sichuan Ruoergai Wetland National Nature Reserve, the changes in landscape patterns over a period of 17 years – from 1990 to 2007 – have been studied by means of RS, GIS technologies and field validation. In the reserve, the seven landscape patterns – river, lake, swamp, seasonal swamp, meadow, shrub and desert – were subject to the current study. The results show that the swamp, seasonal swamp, and meadow are the dominant landscape types occupying over 90% of the reserve’s total area. Over the past 17 years, the distribution area of swamp has been decreased by 3.81%, while that of seasonal swamp and meadow has been increased by 2.58% and 2.09%, respectively. In addition, the desert area has expanded by 1.19% since 2000. The nature reserve can be characterized by patch diversity, causing landscape fragmentation over the years; the total number of patches increased to 585 from 544 and the average area of the patches decreased to 283.49 h m2 from 304.29 h m2 – to the detriment of the wetland functions such as carbon sink and habitats for wild animals. In the study, the causes of the alternations are discussed as mainly resulting from climate change and human disturbances such as overgrazing, drainage, and unmanaged tourism. The study results provide a scientific basis at a strategic scale for the efficient conservation and management implementation of nature reserve zoning and assessment of landscape ecological functions and conservation values.

    • Effects of permafrost degradation on ecosystems

      2010, 30(1):33-39. DOI: 10.1016/j.chnaes.2009.12.006

      Abstract (275) HTML (0) PDF 185.95 K (159) Comment (0) Favorites

      Abstract:Permafrost, covering approximately 25% of the land area in the Northern Hemisphere, is one of the key components of terrestrial ecosystem in cold regions. As a product of cold climate, permafrost is extremely sensitive to climate change. Climate warming over past decades has caused degradation in permafrost widely and quickly. Permafrost degradation has the potential to significantly change soil moisture content, alter soil nutrients availability and influence on species composition. In lowland ecosystems the loss of ice-rich permafrost has caused the conversion of terrestrial ecosystem to aquatic ecosystem or wetland. In upland ecosystems permafrost thaw has resulted in replacement of hygrophilous community by xeromorphic community or shrub. Permafrost degradation resulting from climate warming may dramatically change the productivity and carbon dynamics of alpine ecosystems. This paper reviewed the effects of permafrost degradation on ecosystem structure and function. At the same time, we put forward critical questions about the effects of permafrost degradation on ecosystems on Qinghai–Tibetan Plateau, included: (1) carry out research about the effects of permafrost degradation on grassland ecosystem and the response of alpine ecosystem to global change; (2) construct long-term and located field observations and research system, based on which predict ecosystem dynamic in permafrost degradation; (3) pay extensive attention to the dynamic of greenhouse gas in permafrost region on Qinghai–Tibetan Plateau and the feedback of greenhouse gas to climate change; (4) quantitative study on the change of water-heat transport in permafrost degradation and the effects of soil moisture and heat change on vegetation growth.

    • The validity of burrow counting in estimating the densities of Chiromantes dehaani and Ilyoplax deschampsi in tidal flat at Yangtze Estuary

      2010, 30(1):40-44. DOI: 10.1016/j.chnaes.2009.12.007

      Abstract (260) HTML (0) PDF 394.40 K (393) Comment (0) Favorites

      Abstract:It has been confirmed that the crabs play significant roles in the structure and function of coastal wetland ecosystems, such as mangroves and salt marshes. However it is not easy to estimate the abundance and density of burrowing crabs effectively, thus a further understanding of roles of crabs in these ecosystems has been lagged. Some studies have discussed the suitability of several census techniques, such as burrow counting method in estimating crab density in mangroves. The validities of burrow counting method and other census techniques in estimating crab density, however, has not been tested in salt marshes, especially where vegetation are dense. In this study, we tested the validity of burrow counting method in estimating the densities of Chiromantes dehaani and Ilyoplax deschampsi in tidal flat with dense vegetation of Phragmites australis and Zizania aquatica at Yangtze Estuary through comparing densities estimated by the burrow counting method and the excavation. Burrow counting averagely underestimated the density of C. dehaani by 15% and the degree of underestimation varied among vegetations and habitats (from an overestimate by 23% to underestimate by 41%). Burrow counting averagely overestimated the density of I. deschampsi by 43% and the degree of overestimate varied from 0% to 133% depending on the vegetations and habitats. The percentage of occupied burrows and the number of crabs sharing one burrow were important factors influencing the validity of estimating crab density through burrow counting method.

    • Distribution and interspecific correlation of root biomass density in an arid Elaeagnus angustifolia–Achnatherum splendens community

      2010, 30(1):45-49. DOI: 10.1016/j.chnaes.2009.12.008

      Abstract (242) HTML (0) PDF 331.48 K (149) Comment (0) Favorites

      Abstract:Main objective of this study was to determine the interspecific relationships between two dominant species in terms of root distribution in a typical arid tree-herbage (Elaeagnus angustifolia–Achnatherum splendens) community at Xidatan, Pingluo County, Ningxia Autonomous Region, Northwest China. Eight concentric zones (namely, Z1–Z8) were set from the bases of E. angustifolia individuals to the open lands and five soil profiles were excavated in each zone. Each soil profile was divided into five layers at the depths of 0–10 cm, 10–30 cm, 30–60 cm, 60–100 cm and 100–150 cm. Roots were collected for each species, and soil water content (SWC) and soil bulk density (SBD) were measured for each layer. We found noteworthy roots layer separation in the sub-canopy zones (Z1–Z4). The soil layers with highest fine root biomass density (FRBD) of A. splendens was primarily in the 0–10 cm, which were significantly shallower than those of E. angustifolia; whereas in the inter-canopy zones (Z5–Z8), inconsistent separation, or even overlapping of highest-FRBD-layers emerged between the two dominant species. Correlation analyses showed that negative correlations of FRBD between the two species mainly occurred in those soil layers with relatively higher FRBD and lower SWC. In contrast, positive correlations corresponded with relatively lower FRBD and higher SWC.

Editor in chief:冯宗炜

Inauguration:1981

International standard number:ISSN

Unified domestic issue:CN

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