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Vegetation Development (vegetation + development)
Selected AbstractsThe contribution of geoarchaeology to understanding the environmental history and archaeological resources of the Trent Valley, U.K.GEOARCHAEOLOGY: AN INTERNATIONAL JOURNAL, Issue 2 2005Andy J. Howard This paper provides a review of the contribution that geoarchaeological research has played in elucidating the landscape history of the Trent Valley, U.K. Ameliorating climate in the immediate postglacial led to the expansion of mixed deciduous woodland across the valley floor and the development of an anastomosing channel. In the Lower Trent, fluvial and vegetation development may have been influenced by sea-level change. Around 4000 B.C., the character of the valley floor changed, demonstrated by the dating of tree trunks interbedded within gravel deposits. Synchronicity of changing geomorphological and hydrological processes is suggested, and, while the causal mechanism of this change are not fully understood, tree trunks which were clearly felled have been identified in the valley and provide significant evidence. The later prehistoric and historic archaeological remains, including fishweirs, bridges, and mill dams, point to increasing human activity, and environmental evidence documents the increasing effects of agriculture on the catchment. © 2005 Wiley Periodicals, Inc. [source] Influence of seasonal pressure patterns on temporal variability of vegetation activity in Central SiberiaINTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 3 2006Sergio M. Vicente-Serrano Abstract This paper analyses the spatial distribution of the inter-annual variability of vegetation activity in central Siberia and its relationship with atmospheric circulation variability. We used NOAA-AVHRR NDVI series from Pathfinder Land Data Set at 1° of spatial resolution, and we calculated the annual vegetation activity in each pixel (aNDVI) from 1982 to 2001. Principal component analysis (PCA) was used to determine the general spatial patterns of inter-annual variability of vegetation activity. We identified three main modes, which explain more than 50% of the total variance, each corresponding to a large region. By means of surface pressure grids, we analysed the main patterns of the seasonal atmospheric circulation in the study area: its variability was summarised by means of a few circulation modes and the patterns differ significantly between winter, spring and summer. However, a pattern with a North,South dipole structure represents the general spatial pattern of atmospheric circulation. We investigated the effect of seasonal atmospheric circulation patterns on the inter-annual variation of vegetation activity. In general, the strongest relationships between the atmospheric circulation variability, climate and the aNDVI variability were found in areas where the climatic characteristics are more limiting for the vegetation development, such as the northern regions. This may be explained by the fact that in these areas the variability of atmospheric circulation modes determines summer temperatures, which have a direct impact on vegetation activity. Copyright © 2006 Royal Meteorological Society. [source] Contrasting effects of cattle and wildlife on the vegetation development of a savanna landscape mosaicJOURNAL OF ECOLOGY, Issue 5 2010Kari E. Veblen Summary 1.,Through their effects on plant communities, herbivores can exert strong direct and indirect effects on savanna ecosystems and have the potential to create and maintain savanna landscape heterogeneity. Throughout much of sub-Saharan Africa, periodic creation and abandonment of livestock corrals leads to landscape mosaics of long-term ecosystem hotspots that attract both cattle and large ungulate wildlife. 2.,The development and maintenance of vegetation in these types of hotspots may be controlled in part by herbivory. Cattle and wildlife may have different, potentially contrasting effects on plant succession and plant,plant interactions. We ask how cattle and wild herbivores affect the maintenance and vegetation development of corral-derived landscape heterogeneity (0.25,1.0 ha treeless ,glades') in Laikipia, Kenya, through their effects on long-term successional and short-term plant,plant dynamics. 3.,We used the Kenya Long-term Exclosure Experiment to exclude from glades different combinations of cattle, large ungulate wildlife (i.e. zebras, gazelles and other antelopes), and mega-herbivore wildlife (i.e. giraffes and elephants). We first assessed long-term changes in cover of the dominant grass species, Cynodon plectostachyus and Pennisetum stramineum (the early- and late-dominant species, respectively). We then used a neighbour removal experiment to test the effects of different herbivores on competition and facilitation between the two glade grass species. 4.,In the long-term experiment, we found that large ungulate wildlife reinforced landscape heterogeneity over time by helping maintain glades in their early C. plectostachyus -dominated form. Cattle and mega-herbivore wildlife, on the other hand, appeared to reduce the positive effects through forage preference for C. plectostachyus. 5.,In the neighbour removal experiment, we found that each grass species benefited from facilitation when it was the preferred forage for the dominant grazer. Facilitation of C. plectostachyus by P. stramineum was strongest when cattle co-occurred with wildlife, whereas facilitation of P. stramineum by C. plectostachyus was strongest when cattle were absent. 6.,Synthesis. Our results demonstrate that different combinations of cattle and wildlife have different effects, largely via contrasting forage preferences, on the persistence of landscape heterogeneity in this savanna landscape. More generally, we provide evidence for contrasting effects of cattle and wildlife on short-term plant interactions (facilitation) and successional processes within the herbaceous plant community. [source] Distribution and genesis of Fahlerden (Albeluvisols) in GermanyJOURNAL OF PLANT NUTRITION AND SOIL SCIENCE, Issue 3 2006Peter Kühn Abstract Fahlerden dominate large areas of the young and old moraine landscapes of N and E Germany. Fahlerden (part of Fahlerden corresponds to Albeluvisols) and their transitional subtypes are supposed to have a higher intensity of clay illuviation than Parabraunerden (Luvisols). Besides this macroscopic feature reflecting periglacial influence, micromorphological features such as lenticular platy microstructure, vesicles, and fragments of clay coatings in Bt streaks document the initiation of Fahlerde genesis, which began in the Late Glacial. A model of Fahlerde genesis chronologically connects sedimentological and periglacial processes, vegetation development, and soil-forming processes like decalcification, clay illuviation, and humification. The classification criterion of larger differences in clay contents between E and Bt horizons to distinguish Fahlerden from Parabraunerden needs to be reconsidered, because most Fahlerden have developed in stratified parent material in periglacially influenced landscapes. The interpretation of a soil data base listing data of both soil types distributed in Brandenburg demonstrates that the difference in clay contents between E and Bt horizons may even be smaller in Fahlerden than in Parabraunerden. [source] Assessment of ,13C and C/N ratios in bulk organic matter as palaeosalinity indicators in Holocene and Lateglacial isolation basin sediments, northwest Scotland,JOURNAL OF QUATERNARY SCIENCE, Issue 6 2007Elizabeth A. V. Mackie Abstract Carbon isotopes (,13C) and C/N ratios from bulk organic matter have recently been used as alternative proxies for relative sea-level (RSL) reconstruction where there are problems associated with conventional biological indictors. A previous study on a single isolation basin (Upper Loch nan Eala) in northwest Scotland has shown a clear relationship between ,13C, C/N ratios and palaeosalinity from Younger Dryas and Holocene aged sediments. In this paper we present results of ,13C and C/N ratio analyses from other isolation basins in northwest Scotland over the Holocene and the Lateglacial period in order to validate this technique. The results from the Holocene sequences support the earlier findings that this technique can be used to identify RSL change from isolation basins over the Holocene in this region. The relationship between ,13C, C/N ratios and RSL change is not apparent in sediments of Lateglacial age. Other environmental variables such as atmospheric CO2 concentration, poor vegetation development and temperature influence ,13C values during this period. Copyright © 2007 John Wiley & Sons, Ltd. [source] Spatial patterns of microsite colonisation on two young lava flows on Mount Hekla, IcelandJOURNAL OF VEGETATION SCIENCE, Issue 2 2008N.A. Cutler Abstract Questions: How does vegetation first establish on newly-formed lava substrates? Do very small (cm) and meso-scale (m) variations in the physical environment influence this process and subsequent vegetation development? Location: Mount Hekla, southern Iceland (64°00' N, 19°40' W). Methods: Data on vegetation structure and the incidence of ,safe sites' suitable for colonisation were collected from high and low points on the surfaces of lava flows emplaced during the 1991 and 2000 A.D. eruptions of Mount Hekla. Effects of flow age and meso-topographic position on vegetation structure (moss cover, patch density, stem length) were assessed by two-way analyses of variance. The distributions of colonisation events and available safe sites were analysed using point pattern techniques. Results: Rapid colonisation of the lava surface was observed, despite stressful environmental conditions. The 1991 and 2000 flows differed significantly in vegetation structure, but there were no significant differences in moss cover, patch density and stem length between ,high' and ,low' sites. Conclusions: Colonisation events are invariably associated with small-scale irregularities on the surface of the lava. The colonisation process appears to be spatially random. Development of the moss ,carpet' proceeds by vertical thickening and lateral growth and coalescence of moss patches that establish in ,safe sites'. This process is rapid, with close to 100% of available safe sites exploited within 20 years. Topographic position makes no difference to the very early stages of vegetation development and cannot be used to ,forecast' the later stages of development. [source] Dynamics of grazing lawn formation: an experimental test of the role of scale-dependent processesOIKOS, Issue 10 2008Joris P. G. M. Cromsigt Grazing lawns are characteristic for African savanna grasslands, standing out as intensely grazed patches of stoloniferous grazing-tolerant grass species. Grazing lawn development has been associated with grazing and increased nutrient input by large migratory herds. However, we argue that in systems without mass migrations disturbances, other than direct grazing, drive lawn development. Such disturbances, e.g. termite activity or megaherbivore middens, also increase nutrient input and keep the bunch vegetation down for a prolonged time period. However, field observations show that not all such disturbances lead to grazing lawns. We hypothesize that the initial disturbance has to be of a minimal threshold spatial scale, for grazing intensity to be high enough to induce lawn formation. We experimentally tested this idea in natural tall savanna grassland. We mowed different-sized plots to simulate initial disturbances of different scales (six times during one year) and applied fertilizer to half of the plots during two years to simulate increased nutrient input by herbivores or termite activity. Allowing grazing by naturally occurring herbivores, we followed the vegetation development over more than three years. Grazing kept bunch grass short in coarser, fertilized plots, while grasses grew out toward their initial height in fine-scale and unfertilized plots. Moreover, lawn grasses strongly increased in cover in plots with an increased nutrient input but only after coarser scale disturbance. These results support our hypothesis that an increased nutrient input in combination with grazing indeed induces grazing lawn formation, but only above a threshold scale of the initial disturbance. Our results provide an alternative mechanism for the development of grazing lawns in systems that lack mass migrating herds. Moreover, it gives a new spatial dimension to the processes behind grazing lawn development, and hence help to understand how herbivores might create and maintain spatial heterogeneity in grassland systems. [source] Evaluating the effects of riparian restoration on a temperate river-system using standardized habitat surveyAQUATIC CONSERVATION: MARINE AND FRESHWATER ECOSYSTEMS, Issue S1 2010E. Clews Abstract 1.The restoration of degraded riparian zones to improve a range of functions is attracting increasing interest, but there are still questions about (i) how effectively restoration changes riparian or channel conditions; (ii) whether riparian management offsets the effects of wider catchment pressures; and (iii) whether these effects can be detected quantitatively. 2.A catchment-scale experiment was used to assess the effects of riparian restoration on riparian and channel conditions in the Welsh River Wye. In a hierarchically designed survey, variations in river habitat character were assessed among tributaries where riparian zones were recently managed for restoration (n=9 streams), unmanaged controls (n=12), intensively grazed pastures (n=3) and coniferous plantation (n=3). Management between 1997 and 2003, largely involving coppicing, was designed to exclude grazing through fencing in order to enable vegetation development while creating salmonid refuges. River habitat character was assessed using the UK ,River Habitat Survey' (RHS) method, with habitat variation quantified using Principal Components Analysis. 3.Stream habitats varied significantly among treatment categories. Streams draining plantation conifer had ,harder' channel features, while those draining intensively grazed pasture were characterized by finer substrata and more active channels than elsewhere. Riparian management reduced livestock trampling (= poaching) and increased algal cover relative to controls. Coppicing and riparian fencing successfully excluded grazing on banks while increasing in-stream vegetation cover, but did not affect substrata, flow-types and channel features. 4.These data show that RHS can detect habitat variation among streams in contrasting riparian land-use, revealing some apparently significant effects of recent restoration. We advocate longer-term investigations at reach to catchment scales to assess longer-term effects on channel and flow character, and to appraise fully the extent to which local riparian management can offset impairments at a catchment or larger scale, such as altered run-off regimes, sediment delivery and climate change. Copyright © 2010 John Wiley & Sons, Ltd. [source] Late Weichselian pollen stratigraphy, clay varve chronology and palaeomagnetic secular variations in Lake Bolmen, Småland, south SwedenBOREAS, Issue 3 2001JONAS ISING Pollen analysis, glacial varve chronology and palaeomagnetic measurements were carried out on Late Weichselian lake sediments from southwestern Smaland, south Sweden. The sequence is correlated to the GRIP event stratigraphy, expressed in calendar years BP, and covers the period from the deglaciation at c. 14 400 to 11 300 calendar years BP. The series encompasses c. 930 varves and has been connected to the local varve chronology. Varve thickness increases markedly after the Older Dryas stadial, which indicates an accelerated deglaciation and melting of dead ice. The pollen diagram displays the vegetation development from the deglaciation at c. 14 400 calendar years BP to the transition to the Holocene. The vegetation succession starts with an arctic pioneer vegetation at the deglaciation, changes to a more stable tundra environment and displays a development which concurs with the traditional lateglacial pollen stratigraphy for southern Sweden. A palaeo-magnetic secular variation curve is presented displaying two westerly declination swings at 14200-13800 and 12 800-11 600 calendar years BP, respectively. The upper one can be recognized from other palaeomagnetic stratigraphies from southern Sweden and Estonia. [source] | |||||||||||||