Spatial Representation of Aquatic Vegetation by Macrofossils and Pollen in a Small and Shallow Lake

We have explored the contemporary spatial relationship between aquatic vegetation and surficial macrofossil and pollen remains in a small, shallow, English lake. A detailed point-based (n = 87) underwater vegetation survey was undertaken in the middle of the plant-growing season in July 2000. Then following plant die-back in November 2000, surface sediment samples (upper 1.5 cm) were collected from 30 of these plant survey points and analysed for plant macro-remains (all 30 samples), and pollen (4 evenly spaced samples). All data were stored as separate layers in a geographical information system and spatial relationships between the aquatic vegetation and plant remains were explored. In contrast to pollen types, plant macrofossils were not evenly dispersed across all parts of the lake and, with the exception of Chara oospores, higher concentrations of remains (particularly for Potamogeton) were found close to areas of source-plant dominance. The spatial pattern of macrophyte–macrofossil relationships revealed that vegetative remains (particularly leaf fragments) were probably deposited at source, whereas seeds were recovered close to the shore suggesting slightly wider dispersal. Overall, however, macro-remains best represented local ‘patch-scale’ vegetation within 20–30 m of the core site. The macro-remains effectively recorded the dominant plants in the lake with 63% of samples containing a combination of remains of Chara, Elodea, and Potamogeton. However, relationships between macrophytes and fossils were complex. Some species were significantly over-represented by macrofossils (e.g., Chara spp., Nitella flexilis agg., and Zannichellia palustris), while others were either under-represented (e.g., Potamogeton spp.), or not represented at all (e.g., Lemna trisulca). Pollen represented macrophyte diversity poorly, but some taxa were found (e.g., Myriophyllum spicatum, Ceratophyllum demersum) that were not recorded by macro-remains. We conclude that macrofossil analysis may be very usefully employed to determine the dominant taxa in past aquatic plant communities of shallow, productive lakes and that the addition of pollen analysis provides further information on former species richness.     

First record of myrmecochorous diaspores removal by dung beetles in the Caatinga vegetation,a Brazilian semiarid ecosystem

Canthon (Francmonrosia) carbonarius is recognized as coprophagous and this paper describes, for the first time, the interaction between the dung beetle and seeds of Jatropha mollissima, in Pernambuco state, on the Caatinga vegetation. The observed activities were remotion of elaiosome parts, rolling and deposition of the diaspore on the beetle burial site. Interactions between myrmecochorous diaspores and dung beetle may have important ecological implications. These insects may also act as either predators or secondary dispersal agents of myrmecochorous seeds available in the environment. The findings of the present study serve as a starting point for future studies assessing the ecological implications on the use of this new type of resource by dung beetles in the Caatinga vegetation.     

Aquatic macrophyte dynamics in Lake Karakul (Eastern Pamir) over the last 29 cal ka revealed by sedimentary ancient DNA and geochemical analyses of macrofossil remains

Due to methodological challenges there are only a few studies that focus on macrophyte dynamics in large lakes despite their notable role in a lake’s ecosystem functioning. This study investigates composition and productivity changes of the submerged vegetation of Lake Karakul, Pamir Mountains (Tajikistan), using sedimentary ancient DNA metabarcoding and elemental (C/N) and isotopic (δ¹³C, δ¹⁵N) measurements of Stuckenia cf. pamirica (Baagøe) Z. Kaplan (Potamogetonaceae) leaf remains. No Stuckenia cf. pamirica leaf remains were found for 28.7–26.1 cal ka BP, when both Potamogetonaceae and Chara (L.) DNA sequences were recorded, suggesting sparse submerged vegetation at the coring site. This agrees with the inference of a deep lake reached using geochemical proxies. From 26.1 to 17.5 cal ka BP a few macrophyte remains and high numbers of Potamogetonaceae sequences were recovered: lake level was probably low, as suggested by other studies on the lake. Another phase of increased numbers of Chara sequences and the absence of Stuckenia cf. pamirica leaf remains was found between 17.5 and 12.2 cal ka BP, which coincides with a lake-level transgression at Lake Karakul as indicated by paleo-shoreline investigations. Analyses of macrophyte remains reveal intermediate paleo-productivity from 6.9 cal ka BP and high paleo-productivity from 2.2 cal ka BP onwards. From comparisons with other studies, we suggest that lake-level changes are the main driver for the submerged vegetation composition and productivity at the coring site in Lake Karakul and underline our conclusions by depicting the present-day distribution of Stuckenia cf. pamirica and Chara within the lake.     

Fruit polymorphism in ephemeral species of Namaqualand: IV. Growth analyses of plants cultivated from the dimorphic diaspores

Growth analyses were conducted on two polymorphic annual species, Dimorphotheca sinuata and Arctotis fastuosa of Namaqualand, Republic of South Africa. Plants cultivated from disc diaspores of D. sinuata produced significantly more inflorescences, produced bigger mature plants and allocated more biomass to reproduction than plants cultivated from ray diaspores. Plants of both D. sinuata and A. fastuosa growing on less disturbed sites in the field allocated more biomass to reproduction than plants growing on more disturbed sites. Reproductive allocation of A. fastuosa increased with a decrease in plant size, whereas reproductive allocation was not affected by plant size in the case of D. sinuata.     

Shrubs promote nucleation in the Brazilian semi-arid region

Anthropogenic environmental degradation transforms mature vegetation into sites in succession, and actions to restore these altered environments must be based on ecological theories. Nucleation, promoted by facilitation, is an ecological process that can be applied to the restoration of altered environments. The original vegetation of many semi-arid regions has been profoundly altered, and is difficult to recuperate due to rigorous climates. Observations of secondary succession sites raise the following question: do some semi-arid plant species promote nucleation processes and can they therefore be considered nurse species? To address this question, vegetation surveys were undertaken in different environments: under the canopy of the shrub Combretum leprosum and in adjacent open areas. Shrubs in different stages were classified by canopy size: small, intermediate and large. Diversity and number of seedlings increased as the size of the C. leprosum canopies increased. Some of the environmental variables examined supported the role of C. leprosum as a facilitator species, such as the improvement in soil conditions under its canopy. Thus C. leprosum could be of significant importance in restoring degraded areas of the semi-arid region where it is present, by allowing the establishment of other plant species.     

南洛河流域洛南盆地表土孢粉与植被的关系(英文)

The catchment of South Luohe River in Central China is an important region for investigating modern pollen-environment relationship, because it is located in the transitional zone between south and north China, an environment which is sensitive to climate changes. In this study, 40 surface samples under ten vegetation types were collected to reveal the relationship between pollen assemblages and vegetation. The results show that the surface pollen assemblages reflect the vegetation quite well. In forest topsoils, the average of arboreal pollen content is greater than 40%, and the Selaginella sinensis spore is high. As to sparse forest grassland and shrub community, the average arboreal pollen is 13.2% and 16.6% respectively, and the shrub pollen is relatively higher than that of grassland samples. The grassland and farmland are characterized by low percentage of tree and shrub pollen(<10% and <1%), and high percentage of herbs(>80%). Pinus, Quercus and some other arboreal pollen can indicate the regional vegetation because of their dispersal ability. Quercus pollen is under-representative and so is Pinus. Artemisia pollen is significantly over-represented, has poor correlation with the plant coverage, and may reflect human disturbance. Gramineae can indicate plant quite well, but with low representation. High content of Chenopodiaceae probably suggests human impact. Predominant Selaginella sinensis can be used as an indicator of forest environment. Cluster analysis and principal components analysis of pollen assemblages can distinguish forest and non-forest vegetation well. The former method is better at separating pine and mixed forests, while the latter is more stable and could better differentiate farmland and other non-forest area. The first axis of PCA mainly reflects the humidity.     

Seedling recruitment in a semi-arid steppe: The role of microsite and post-dispersal seed predation

Grasslands dominated by Stipa tenacissima are important ecosystems in the arid and semiarid climates of western Mediterranean, where they have originated by degradation of open dry forests and shrublands. At present, although the level of exploitation in these ecosystems is very low, succession processes seem to have stopped. In this study, we explore the role of microsite and post-dispersal seed predation on the seedling emergence of two species from advanced successional stages (Rhamnus lycioides, Quercus coccifera), three species from degraded stages (Cistus clusii, Helianthemum violaceum, Anthyllis terniflora), and of the dominant species (Stipa tenacissima). Seeds of these species were sown in plots divided into two microsites: (i) under tussocks of S. tenacissima and (ii) in the bare soil between tussocks. Soil moisture was significantly higher in the tussock microsites. The interaction observed between microsite and time, reflected the slower drying process under tussocks. Seed predation was in general high and differed significantly between species but not between microsites. Q. coccifera was especially affected by predation. The only germination detected in gap areas was that of H. violaceum. The results pointed to a direct facilitative effect of tussock grass on the germination in R. lycioides (20.4±8.0%) and S. tenacissima (41.3±5.7%) while the corresponding figures for bare ground were 0%. These results suggest that the recovery of potential vegetation in this ecosystem is not possible or, at least, is very slow because the residual shrub patches do not generate a sufficient number of seeds able to disperse to favorable germination microsites. S. tenacissima may act as facilitator of seedling recruitment if there is a supply of diaspores.     

Vegetation and soil characteristics of the wasteland of Valika Chemical Industries near Manghopir, Karachi

The vegetation of the wasteland of Valika chemical industries near Manghopir road, Karachi was studied. Nine plant communities were recognized based on dominant species. In these plant communities the vegetation was disturbed, mostly halophytic and dominated bySuaeda fruticosa,Tamarix indica,Salsola baryosma,Cressa cretica,Atriplex griffithii,Haloxylon recurvum,Indigofera hochstetteri,Prosopis julifloraandChenopodium album.The physico-chemical properties of the soils were also analysed. Soil texture was mostly sandy loam, which exhibited slight variations in the water-holding capacity. The soils contained a sufficient amount of CaCO₃⁻and exhibited mostly alkaline soil pH. The soils of the different plant communities had scarcely any organic matter or inorganic phosphorus. The exchangeable sodium in the soils of many halophytic plant communities was high, with appreciable concentrations of potassium.     

Vegetation of dune sands of Olkhon Island on Baikal and some questions concerning its protection

The need for the conservation of vegetation on dune sands of Olkhon Island is substantiated. Psammophytic phytocenoses evolving on the sands are of rare occurrence, in their composition, structure and spread, for the Prebaikalia. Endemic and relict plant species constitute a rarity core of the flora of these cenoses. The state protection method for several tracts of sand landscape is suggested for biodiversity sustenance on the island.     

Trophic preferences in an assemblage of mammal herbivores from Andean Puna (Northern Chile)

The patterns of plant consumption and preference were assessed for three mammal herbivores, the rodents Abrocoma cinerea and Chinchilla brevicaudata, and the camelid Vicugna vicugna, co-occurring in the Andean Puna (Chile). The plant proportion in the diet estimated from faeces epidermic materials was compared to transect plant cover. Although the harsh climatic conditions constrained plant availability (low vegetation, xerophytic species rich in secondary metabolites and structural carbohydrates) none of the mammals consumed plants according to their availability, displaying adaptations for efficient plant processing. V. vicugna, with a broad trophic niche, consumed short grasses and secondarily shrubs; C. brevicaudata also combined herbaceous plants and shrubs; and A. cinerea was specialised in shrub-eating. Although trophic overlap between the first two species was moderate, interactions were minimised by the mobility and low-impact grazing of V. vicugna. It is suggested that the diet of the three species differed due to their dissimilar abilities for responding to concentrations of secondary metabolites. The plants preferred by C. brevicaudata and V. vicugna did not carry high nutritional content but rather low content of secondary compounds. Conversely, A. cinerea was able to excrete terpenes, with metabolic costs compensated by the high energetic content of the plants eaten.     

Variation in the moisture regime of northeastern interior Alaska and possible linkages to the Aleutian Low: inferences from a late-Holocene δ18O record

Analyses of oxygen and carbon isotopes in bulk carbonate and Chara-stem encrustations, X-ray diffraction, and sediment composition from Keche Lake offer new information on climatic change over the past ~3,400?years in northeastern interior Alaska. The ??¹⁸O and ??D values of water samples from the lake and its inlet streams suggest that evaporation plays an important role in determining the isotopic composition of Keche Lake water at present. However, evaporative enrichment does not appear to be a major driver of the pronounced fluctuations in the bulk-carbonate ??¹⁸O record on the basis of comparison with Chara-??¹⁸O values. The ??¹⁸O values of bulk carbonate in the Keche Lake sediments vary by up to 10??? over the past 3,400?years, with maximum values of ?12??? around 3,400?cal BP and between 2,100 and 1,500?cal BP. High ??¹⁸O peaks are associated with sediments dominated by quartz, feldspar, and clay minerals suggesting the influence of detrital carbonate. Multi-millennial patterns of ??¹⁸O variation at Keche Lake appear to be linked with changes in watershed and sediment-depositional processes, which may be driven by varying moisture abundance associated with the position of the Aleutian Low (AL). The increasing trend of carbonate ??¹⁸O from 3,400 to ~2,100?cal BP probably reflects the increasing importance of a westerly AL, and the high frequency of ??¹⁸O spikes ~2,100?C1,500?cal BP may have resulted from the prevalence of a westerly AL position. Predominance of a westerly AL likely increased snowfall and winter temperature in the region. Such conditions would have promoted soil erosion and thermokarst activity during spring snowmelt, resulting in episodic large influxes of detrital carbonate to Keche Lake and elevating bulk-carbonate ??¹⁸O. Over the past 1,500?years, bulk-carbonate ??¹⁸O remained relatively high at Keche Lake but variation was much less pronounced than before. A broad ??¹⁸O peak centered ~400?cal BP may be related to enhanced winter moisture during the Little Ice Age, although our chronology is inadequate for a rigorous assessment of this interpretation. This study contributes a new ??¹⁸O record and offers additional information on past moisture-regime shifts associated with changing atmospheric-circulation patterns.     

塔里木河下游常见植物繁殖体形态特征比较

4- 以塔里木河下游荒漠河岸林21种常见植物繁殖体为研究对象,对其形态特征进行了比较分析.结果表明:(1)不同繁殖体之间重量差别很大.单粒重最小的是多花柽柳(0.019 8 mg),最大的是沙枣(131.387 2 mg);(2)繁殖体三维(长、宽、高)的方差最小的是胀果甘草(0.022),方差最大的是蒲公英0.145.菊科、禾本科、茄科和荚竹桃科植物繁殖体均偏离圆球形较大(方差>0.05);(3)柽柳科、杨柳科、菊科和夹竹桃科均具有附属物,这些形态特征有利于物种的扩散和定居;(4)有7种植物的繁殖体重量小于1 mg,且比较接近圆球形(方差小于0.09),有利于形成持久土壤种子库.     

Subfossil Cladocera from surface sediment in thermokarst lakes in northeastern Siberia,Russia, in relation to limnological and climatic variables

Subfossil Cladocera were sampled and examined from the surface sediments of 35 thermokarst lakes along a temperature gradient crossing the tree line in the Anabar-river basin in northwestern Yakutia, northeastern Siberia. The lakes were distributed through three environmental zones: typical tundra, southern tundra and forest tundra. All lakes were situated within the continuous permafrost zone. Our investigation showed that the cladoceran communities in the lakes of the Anabar region are diverse and abundant, as reflected by taxonomic richness, and high diversity and evenness indices (H = 1.89 ± 0.51; I = 0.8 ± 0.18). CONISS cluster analysis indicated that the cladoceran communities in the three ecological zones (typical tundra, southern tundra and forest-tundra) differed in their taxonomic composition and structure. Differences in the cladoceran assemblages were related to limnological features and geographical position, vegetation type, climate and water chemistry. The constrained redundancy analysis indicated that T_July, water depth and both sulphate (SO₄ ^2?) and silica (Si⁴⁺) concentrations significantly (p ≤ 0.05) explained variance in the cladoceran assemblage. T_July featured the highest percentage (17.4 %) of explained variance in the distribution of subfossil Cladocera. One of the most significant changes in the structure of the cladoceran communities in the investigated transect was the replacement of closely related species along the latitudinal and vegetation gradient. The results demonstrate the potential for a regional cladoceran-based temperature model for the Arctic regions of Russia, and for and Yakutia in particular.     

The relation between accessibility,diversity and indigenous valuation of vegetation in the Bolivian Andes

A quantitative ethnobotanical study was conducted in the semi-arid Bolivian Andes community of Apillapampa to evaluate the impact of site accessibility on the diversity and perceived usefulness of (sub-)woody plants. Vegetation was sampled in thirty-six transects of 50 × 2 m², whereas data on plant uses were obtained from 13 local Quechua participants. Accessibility of sample sites correlated negatively with plant diversity, but positively with perceived usefulness. Hence, in spite of being less diverse, vegetation of more accessible sites was perceived as more useful to people than vegetation of more remote and also more diverse sites. This result contributes to the validity of the widely accepted notion that “more accessible plant resources are more useful to people”, not only at the level of individual plant species, but also for entire vegetation communities. In this respect, our finding that people attribute an equal usefulness to the vegetation of two local ecological zones (i.e. prepuna and puna) most likely reflects their similar accessibility from the village centre, which is located on the edge between both zones.     

Spatial and temporal characteristics of Neogene palynoflora in China and its implication for the spread of steppe vegetation

This study reviews 17 published Neogene pollen records with independent age control to provide a better understanding of the vegetation evolution and climate change in China, especially of the past shifts of the arid–semiarid steppe. During the late Early Miocene to early Middle-Miocene period, most of East and South China was covered by woodland vegetation (e.g., Quercus, Carya, Alnus, and Juglans) while Northwest China was mainly steppe (e.g., Artemisia), generally indicating a warm and humid climate influenced by a strong East-Asian summer monsoon. Since the Early Miocene the vegetation boundary between both regions has moved through time as the climate has changed. During the late Middle to Late Miocene cooling, herbs and shrubs increased significantly in the vast region north to the Yangtze River of South China and major woodland vegetation retreated to south of the Yangtze River. In the context of this cooling, a drier season probably became established north to the Yangtze River, as is evident from the late Middle Miocene to Pliocene compiled palynoflora data. Nevertheless, a little resumption for woodland vegetation occurred during the Early Pliocene in North China, presumably corresponding to global climate amelioration. Thus, the stepwise declining pattern of modern vegetation distribution from southeast to northwest in China can be traced back to at least the late Middle Miocene. In the meanwhile, the Neogene vegetation and its inferred climate history in China indicated a general declining trend of East-Asian summer monsoon.     

Influence of soil, tree cover and large herbivores on field layer vegetation along a savanna landscape gradient in northern Botswana

The response of the field layer vegetation to co-varying resource availability (soil nutrients, light) and resource loss (herbivory pressure) was investigated along a landscape gradient highly influenced by elephants and smaller ungulates at the Chobe River front in Botswana. TWINSPAN classification was used to identify plant communities. Detrended Correspondence Analysis (DCA) and Canonical Correspondence Analysis (CCA) were used to explore the vegetation-environment relationships. Four plant communities were described: Panicum maximum woodland, Tribulus terrestris woodland/shrubland, Chloris virgata shrubland and Cynodon dactylon floodplain. Plant height, species richness and diversity decreased with increasing resource availability and resource loss. The species composition was mainly explained by differences in soil resources, followed by variables related to light availability (woody cover) and herbivory, and by interactions between these variables. The vegetation structure and species richness, on the other hand, followed the general theories of vegetation responses to herbivory more closely than resource related theories. The results suggest a strong interaction between resource availability and herbivory in their influence on the composition, species richness and structure of the plant communities.     

Effective environmental factors in the distribution of vegetation types in Poshtkouh rangelands of Yazd Province (Iran)

The objective of this research was to study the relationships between environmental factors and vegetation in order to find the most effective factors in the separation of the vegetation types in Poshtkou rangelands of Yazd province. Sampling of soil and vegetation were performed with randomized-systematic method. Vegetation data including density and cover percentage were estimated quantitatively within each quadrat, and using the two-way indicator species analysis (TWINSPAN), and vegetation was classified into different groups. The topographic conditions were recorded in quadrat locations. Soil samples were taken in 0–30 and 30–60 cm depths in each quadrat. The measured soil variables included texture, lime, saturation moisture, gypsum, acidity (pH), electrical conductivity, sodium absorption ratio, and soluble ions (Na⁺, K⁺, Mg²⁺, Cl⁻, CO₃²⁻, HCO₃⁻ and SO₄²⁻). Multivariate techniques including principal component analysis (PCA) and canonical correspondence analysis (CCA) were used to analyse the collected data. The results showed that the vegetation distribution pattern was mainly related to soil characteristics such as salinity, texture, soluble potassium, gypsum, and lime. Totally, considering the habitat conditions, ecological needs and tolerance range each plant species has a significant relation with soil properties.     

Lake-Level Fluctuations and Small-Scale Vegetation Patterns During the Late Glacial in The Netherlands

Late glacial changes in the vegetation were studied in and around a former lake on the southeastern side of a coversand ridge near Milheeze (southern Netherlands). Analyses of microfossils and macroremains and AMS ¹⁴C dating were performed on four sediment cores along a transect from sand ridge to the lake centre. Small-scale vegetation patterns and lake-level fluctuations were reconstructed in detail based on the information provided by the transect. For the first time in The Netherlands, cores along a transect within one lake were used to reconstruct the amplitude of late glacial lake-level fluctuations. Near Milheeze, a small and shallow lake was formed during the Bølling. The large increase in the water level during the Bølling and early Allerød, and the transition to more eutrophic conditions at the start of the Allerød, were probably related to the disappearance of permafrost. During the Allerød, open birch and pine woodlands developed in the area. In the lake, organic deposits accumulated, and the lake size and depth fluctuated. At the start of the Younger Dryas, higher lake water levels were recorded and woodlands became more open as a result of both a drop in the temperature and an increase in the effective precipitation. During the late Younger Dryas the lake water level dropped as the climate became drier and temperatures slightly increased. Accumulation of organic deposits in the lake ceased at the end of the Younger Dryas, which was caused by a drop in the water level in combination with the hydroseral succession process within the lake itself. The climatic signal reflected in the late glacial flora and lake-level fluctuations agree well with other published data from The Netherlands.     

Patterns of seed occurrence in corsac and red fox diets in Mongolia

Corsac fox (Vulpes corsac) and red fox (Vulpes vulpes) diets often consist of small quantities of vegetation, including fruit and seeds that may represent important sources of energy and nutrition. However, details of the species consumed are few, but may provide insight into the role of foxes as seed dispersers. We analyzed scats of corsac (n = 408) and red foxes (n = 533) collected in an arid region of Mongolia from June 2006 to June 2007. We found 13 seed species in corsac scats, the most common being Allium polyrhizum, Asparagus gobicus, and Tribulus terrestris, and 12 species in red fox scats, the most common being Amygdalus pedunculata, Corispermum mongolicum, and T. terrestris. The proportion of scats with seeds varied significantly by season for both foxes. Seeds occurred most frequently during the breeding period, which corresponded with winter, and least frequently during the dispersal period in autumn for both species. We detected no differences in the proportion of scats with seeds between species seasonally. Our results suggest that fruit represents an important component of diet, especially during winter when availability of other prey items is low, and that both foxes may facilitate seed dispersal of some plant species.     

Climate conditions and relative abundance of C<Subscript>3</Subscript> and C<Subscript>4</Subscript> vegetation during the past 40 ka inferred from lake sediments in Wudalianchi,northeast China

Paleoclimate and paleovegetation changes over the last 40 cal ka were recorded by multiple variables in a sediment core from Qingshi, Wudalianchi City, northeast China. The history of vegetation types inferred from n-C₂₇/n-C₃₁ and average chain length of n-alkanes indicates the paleovegetation went through several distinct stages, consistent with pollen records from the study area. Compound-specific carbon isotope composition was also determined for C₂₇, C₂₉ and C₃₁ n-alkanes in the Qingshi core sediments. The relative abundance of C₃ and C₄ plants was calculated using a binary model and indicates that C₃ plants were the dominant input during the last glacial and Holocene. There were, however, shifts in the ratio of C₃ to C₄ vegetation abundance that correspond to changes in climate conditions. Generally, the long-term trend towards greater C₄ plant abundance from the last glacial to Holocene correlated with an increase in pCO₂, higher temperature, greater precipitation and more growing season precipitation. Our results suggest that temperature and seasonality of precipitation played a strong role in altering the relative abundance of C₃ and C₄ plants in the study area. These results provide information for predicting future vegetation changes in response to on-going global warming.