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81.
定居是人类从高度移动的游猎生活发展到全年固定于一处居住的漫长过程。定居的发生和发展对人类社会的生产方式、技术演化和文明起源具有深远影响,而定居的产生受到气候变化、人口增长、资源压力、技术革新等多种因素影响。青藏高原是研究人类适应和定居高寒缺氧极端环境的理想区域,对史前人类在青藏高原的定居过程关注较多亦争议颇多。通过梳理已发表的考古学、地理学、遗传学等相关学科文献,发现目前对于史前人类定居青藏高原的研究,侧重于讨论低海拔人群或者农作物扩散的影响,对动物资源在这一过程中的作用则关注较少,定居高原的年代和驱动机制仍存在争议。遗址使用的季节性分析,是判断古人是否全年定居的关键。本文总结了如何利用青藏高原鱼类、鸟类和哺乳类等动物遗存因地制宜进行遗址季节性分析以及建立高原遗址动物资源利用时间表的方法。本文认为,开展史前人类在青藏高原定居与动物资源利用研究,首先,应全面建立和完善青藏高原现生动物骨骼形态、全基因组和蛋白质组的数据库,为考古遗址动物遗存物种鉴定提供基础;其次,在物种鉴定的基础上,研究人—动物—环境之间的关系;最后,评估人类在遗址活动的季节性以及动物资源在人类定居青藏高原过程中的作用。  相似文献   
82.
Spatial and temporal variability of hydrological responses affecting surface water dissolved organic carbon (DOC) concentrations are important for determining upscaling patterns of DOC export within larger catchments. Annual and intra‐annual variations in DOC concentrations and fluxes were assessed over 2 years at 12 sites (3·40–1837 km2) within the River Dee basin in NE Scotland. Mean annual DOC fluxes, primarily correlated with catchment soil coverage, ranged from 3·41 to 9·48 g m?2 yr?1. Periods of seasonal (summer–autumn and winter–spring) DOC concentrations (production) were delineated and related to discharge. Although antecedent temperature mainly determined the timing of switchover between periods of high DOC in the summer‐autumn and low DOC in winter‐spring, inter‐annual variability of export within the same season was largely dependent on its associated water flux. DOC fluxes ranged from 1·39 to 4·80 g m?2 season?1 during summer–autumn and 1·43 to 4·15 g m?2 season?1 in winter–spring.Relationships between DOC areal fluxes and catchment scale indicated that mainstem fluxes reflect the averaging of highly heterogeneous inputs from contrasting headwater catchments, leading to convergent DOC fluxes at catchment sizes of ca 100 km2. However, during summer–autumn periods, in contrast to winter–spring, longitudinal mainstem DOC fluxes continue to decrease, most likely because of increasing biological processes. This highlights the importance of considering seasonal as well as annual changes in DOC fluxes with catchment scale. This study increases our understanding of the temporal variability of DOC upscaling patterns reflecting cumulative changes across different catchment scales and aids modelling of carbon budgets at different stages of riverine systems. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   
83.
This study reports the seasonal variability in aspects of the physiology of the shore crab Carcinus maenas from three estuaries in South-west England, each with varying anthropogenic inputs: Avon Estuary (‘relatively low’ impact), Yealm Estuary (‘intermediate’ impact) and Plym Estuary (‘relatively high’ impact). Crabs collected over 12 months from the Avon had a significantly ‘lower’ physiological condition in winter and spring compared to summer and autumn; in particular, haemocyte phagocytic capability (a general indicator of immune function) was significantly higher in winter and spring compared to summer and autumn, and total haemolymph antioxidant status (an indicator of oxidative stress) was significantly lower in winter compared to the remainder of the year. Potentially, shore crabs may be more susceptible to the effects of contaminant exposure, such as increased immunotoxicity (thus, reduction of immune function) and/or oxyradicals (or reactive oxygen species) exposure) especially in seasons of increased susceptibility i.e. summer/autumn (lower phagocytic capability) and winter (lowest antioxidant function). As the Avon was taken to represent the ‘reference’ site, this pattern is considered to reflect the ‘normal’ seasonal variability in shore crab physiology. Shore crab physiological condition from the ‘relatively high’ impact estuary (Plym) revealed increased cellular viability and antioxidant status in autumn and winter compared with that of the ‘standard’ pattern (Avon) However, crabs from the intermediate impact estuary (Yealm) only demonstrated significant physiological differences in summer as shown by a lower cellular viability. All crabs had been exposed to PAHs (confirmed by the presence of PAH metabolites in their urine) which may account for the observed differences in shore crab physiology. In conclusion, to aid understanding of the potential contaminant impacts on biota it is imperative that the ’normal’ seasonal variability of physiological condition be established. Biological effects-based monitoring studies should therefore be employed seasonally to potentially highlight ‘windows of sensitivity’ to contaminant impact.  相似文献   
84.
Recent variations in the precipitation regime across southern Europe have led to changes in river fluxes and salinity gradients affecting biological communities in most rivers and estuaries. A sampling programme was developed in the Mondego estuary, Portugal, from January 2003 to December 2008 at five distinct sampling stations to evaluate spatial, seasonal and inter-annual distributions of fish larvae. Gobiidae was the most abundant family representing 80% of total catch and Pomatoschistus spp. was the most important taxon. The fish larval community presented a clear seasonality with higher abundances and diversities during spring and summer seasons. Multivariate analysis reinforced differences among seasons but not between years or sampling stations. The taxa Atherina presbyter, Solea solea, Syngnathus abaster, Crystallogobius linearis and Platichthys flesus were more abundant during spring/summer period while Ammodytes tobianus, Callionymus sp., Echiichthys vipera and Liza ramada were more abundant in autumn/winter. Temperature, chlorophyll a and river flow were the main variation drivers observed although extreme drought events (year 2005) seemed not to affect ichthyoplankton community structure. Main changes were related to a spatial displacement of salinity gradient along the estuarine system which produced changes in marine species distribution.  相似文献   
85.
The dynamics of snow cover is considered an essential factor in phenological changes in Arctic tundra and other northern biomes. The Moderate Resolution Imaging Spectroradiometer (MODIS)/Terra satellite data were selected to monitor the spatial and temporal heterogeneity of vegetation phenology and the timing of snow cover in western Arctic Russia (the Yamal Peninsula) during the period 2000-10. The magnitude of changes in vegetation phenology and the timing of snow cover were highly heterogeneous across latitudinal gradients and vegetation types in western Arctic Russia. There were identical latitudinal gradients for "start of season" (SOS) (r2 = 0.982, p<0.0001), "end of season" (EOS) (r2 = 0.938, p<0.0001), and "last day of snow cover" (LSC) (r2 = 0.984, p<0.0001), while slightly weaker relationships between latitudinal gradients and "first day of snow cover" (FSC) were observed (r2 = 0.48, p<0.0042). Delayed SOS and FSC, and advanced EOS and LSC were found in the south of the region, while there were completely different shifts in the north. SOS for the various land cover features responded to snow cover differently, while EOS among different vegetation types responded to snowfall almost the same. The timing of snow cover is likely a key driving factor behind the dynamics of vegetation phenology over the Arctic tundra. The present study suggests that snow cover urgently needs more attention to advance understanding of vegetation phenology in the future.  相似文献   
86.
Abstract

It is widely accepted that natural resources should only be sustainably exploited and utilized to effectively preserve our planet for future generations. To better manage the natural resources, and to better understand the closely linked Earth systems, the concept of Digital Earth has been strongly promoted since US Vice President Al Gore's speech in 1998. One core element of Digital Earth is the use and integration of remote sensing data. Only satellite imagery can cover the entire globe repeatedly at a sufficient high-spatial resolution to map changes in land cover and land use, but also to detect more subtle changes related for instance to climate change. To uncover global change effects on vegetation activity and phenology, it is important to establish high quality time series characterizing the past situation against which the current state can be compared. With the present study we describe a time series of vegetation activity at 10-daily time steps between 1998 and 2008 covering large parts of South America at 1 km spatial resolution. Particular emphasis was put on noise removal. Only carefully filtered time series of vegetation indices can be used as a benchmark and for studying vegetation dynamics at a continental scale. Without temporal smoothing, subtle spatio-temporal patterns in vegetation composition, density and phenology would be hidden by atmospheric noise and undetected clouds. Such noise is immanent in data that have undergone solely a maximum value compositing. Within the present study, the Whittaker smoother (WS) was applied to a SPOT VGT time series. The WS balances the fidelity to the observations with the roughness of the smoothed curve. The algorithm is extremely fast, gives continuous control over smoothness with only one parameter, and interpolates automatically. The filtering efficiently removed the negatively biased noise present in the original data, while preserving the overall shape of the curves showing vegetation growth and development. Geostatistical variogram analysis revealed a significantly increased signal-to-noise ratio compared to the raw data. Analysis of the data also revealed spatially consistent key phenological markers. Extracted seasonality parameters followed a clear meridional trend. Compared to the unfiltered data, the filtered time series increased the separability of various land cover classes. It is thus expected that the data set holds great potential for environmental and vegetation related studies within the frame of Digital Earth.  相似文献   
87.
利用1961~ 2007年NCEP/NCAR的再分析逐日资料,分析高原主体上空大气环流的季节变化和受到高原影响的东亚大型环流系统的季节变化,以此证明本文得到的“高原普适性划分方法”的合理性.得到的初步结论概括如下:高原主体上空的位势高度、风场、高空温度、降水的季节变化和高原普适性季节划分方法划分的高原四季变化一致,高原南亚高压、副热带高压、副热带西风急流的三个特征指数季节变化和高原普适性季节划分方法划分的高原四季变化一致,这些结论都说明高原普适性季节划分方法划分的高原四季是合理的;风场季节率(500hPa、100hPa)显著区随高度升高向赤道靠近,风场季节率的变化主要和东亚季风的变化有关,大气环流系统季节率的显著说明了大气环流的季节变化,同时也证明了高原普适性季节划分方法的合理性.  相似文献   
88.
The unbalanced submesoscale motions and their seasonality in the northern Bay of Bengal(BoB) are investigated using outputs of the high resolution regional oceanic modeling system. Submesoscale motions in the forms of filaments and eddies are present in the upper mixed layer during the whole annual cycle. Submesoscale motions show an obvious seasonality, in which they are active during the winter and spring but weak during the summer and fall. Their seasonality is associated with the mixed layer...  相似文献   
89.

Although acts of creation, scientific or artistic, result from metaphorical and mythological speculations, the role of metaphor and myth has largely been neglected in attempts to develop a geographical epistemology. The significance of these concepts is illustrated by the use of the frontier symbol as a means of understanding both the social structure of the contemporary black inner city and the temporal dimension of the recent expansion of human activities into nighttime.  相似文献   
90.
Freshwater macroinvertebrate data collected from streams in Taranaki, New Zealand (1981–2006) were used to examine seasonality of biological indices including taxon richness, %EPT (Ephemeroptera, Plecoptera, and Trichoptera) richness, and the hard‐ and soft‐bottomed (‐sb) stream versions of the Macroinvertebrate Community Index (MCI). All indices tested showed modest but statistically significant seasonal variation in hard‐bottomed streams. Seasonal means for the MCI were within ±3.0% of the annual mean. The Semi‐Quantitative MCI (SQMCI) (±4.3%), %EPT richness (±7.4%) and taxon richness (±7.7%) showed greater seasonal variability than the MCI. MCI, SQMCI, and %EPT richness were significantly higher in spring and winter compared with autumn and summer. Taxon richness was lower in winter than in other seasons. In soft‐bottomed streams, SQMCI‐sb showed least seasonality (within ±3.6% of the annual mean, nonsignificant), followed by MCI‐sb and taxon richness (±4.7%), and %EPT richness (±11.2%). Spring and winter MCI‐sb and SQMCI‐sb values tended to be significantly higher than those calculated from summer or autumn samples, although most values were within 5% of the annual site means. Examination of seasonal variation in species traits and their relationships to observed seasonal patterns of biotic indices did not support the suggestion that seasonal variations in life histories of aquatic macroinvertebrates affect index values. Rather, seasons with higher biotic index values were associated with a greater frequency of flow disturbance, which is consistent with the view that the character of New Zealand's stream macroinvertebrate communities with their poorly‐synchronised life histories, has been shaped by the unpredictable physical environment. We recommend the MCI and MCI‐sb for State of Environment reporting in New Zealand for cost‐effectiveness and because data requirements and seasonal variation were less than for quantitative alternative indices. We suggest that seasonal variability is unlikely to confound interpretation, and does not need to be considered.  相似文献   
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