Characterizing and assessing key ecosystem services in a representative forest ecosystem in Turkey

Characterizing and managing multiple ecosystem services is vital for decision-making in sustainable forest management. This study focuses on characterizing and assessing the biophysical and spatial distribution of ecosystem services such as wood production, biodiversity and carbon sequestration in the Kumluca state forest (Turkey). The key ecosystem services were thematically characterized, economically valued, spatially mapped and mobilized as a knowledge-base for ecosystem based planning. Average wood production is higher (135.06 m³/ha) than the overall average (72 m³/ha) in Turkey. The average carbon stock is 119 tC/ha, indicating a medium capacity. The habitat potential for biodiversity is low to medium, based on the 15 target species. Total economic value of the key ecosystem services is estimated at US$624,748,191 (US$6132/ha). The composition and spatial distribution of vegetation determines the extent and potential of ecosystem services. This study emphasizes that comprehensive quantification as well as valuation of ecosystem services can facilitate underpinnings for efficient communication and good decision making in sustainable resource management for multiple values. The orchestrated vision of conservation and sustainable use of ecosystem services based on a comprehensive characterization, modeling, valuing and participatory approach is a strategy for sustainable forest management.     

Biogeochemistry of a gypsum-encrusted microbial ecosystem

Gypsum crusts containing multicolored stratified microbial populations grow in the evaporation ponds of a commercial saltern in Eilat, Israel. These crusts contain two prominent cyanobacterial layers, a bright purple layer of anoxygenic phototrophs, and a lower black layer with active sulphate reduction. We explored the diel dynamics of oxygen and sulphide within the crust using specially constructed microelectrodes, and further explored the crust biogeochemistry by measuring rates of sulphate reduction, stable sulphur isotope composition, and oxygen exchange rates across the crust–brine interface. We explored crusts from ponds with two different salinities, and found that the crust in the highest salinity was the less active. Overall, these crusts exhibited much lower rates of oxygen production than typical organic‐rich microbial mats. However, this was mainly due to much lower cell densities within the crusts. Surprisingly, on a per cell‐volume basis, rates of photosynthesis were similar to organic‐rich microbial mats. Due to relatively low rates of oxygen production and deep photic zones extending from 1.5 to 3 cm depth, a large percentage of the oxygen produced during the day accumulated into the crusts. Indeed, only between 16% to 34% of the O₂ produced in the crust escaped, and the remainder was internally recycled, used mainly in O₂ respiration. We view these crusts as potential homologs to ancient salt‐encrusted microbial ecosystems, and we compared them to the 3.45 billion‐year‐old quartz barite deposits from North Pole, Australia, which originally precipitated gypsum.     

Productivity relations in a Carex-dominated ecosystem

Summary Seasonal and total primary productivity was measured for a Carex meadow in southern Quebec, Canada. Forty-five one-meter² plots were sampled for dry weight biomass, species composition, structure (species density, diversity, height) and soil parameters including macronutrient concentrations (Ca, K, Mg, Na, N, P), pH, organic matter, and water depth. Shoot net productivity and litter decomposition rates were computed for 20-day intervals May–September, inclusive. Relationships between all parameters were examined by principal components analysis.Dominant species included Carex lacustris, C. aquatilis, Calamagrostis canadensis, and Typha angustifolia. For a 130-day growth period, mean shoot net productivity was 6.3 g·m^-2· da^-1 and terminal standing crop 807 g·m^-2. Terminal standing crop was very close to above ground biomass predicted by the Gorham equation based on thermal relations for Carex ecosystems and to total accumulated litter mass (779 g·m^-2). Seasonal production showed a strong bimodal pattern with peak productivities in mid-June (15.3 g·m^-2·da^-1) and mid-July (4.3 g·m^-2·da^-1). Decomposition of the previous year's litter was 81% complete by late September.Soil fertility, fire incidence, and topographic position were the three most important gradients resolved by principal components analysis. The first component distinguished sediment-rich Typha angustifolia communities near open water from oligotrophic stands of Carex spp. on central areas of the meadow. Production levels correlated closely with extractable soil calcium (r=0.40^**) and phosphorus levels (r=0.39^**). Species diversity and stem density related inversely to productivity on this component. Fire incidence (component II) had a marked effect on species diversity due to surface scarification and removal of litter mass. Component III was a topographic gradient separating composition, and community structure.Magnesium and sodium levels decreased from upland to open water. Soil phosphorus increased markedly at water's edge related to mineral input by sedimentation. Pattern of N, P, K, and Ca coincided closely with total shoot production and litter mass levels suggesting closed biotic cycles of these elements.A model accounting for species diversity levels in Carex meadow was formulated based on the assumption that high productivity results in competitive species elimination.     

高校校园生态系统可控性

在环境问题日趋严重的背景下,人类一直在探索将城市生态系统改造成能够自身循环、更好利用可再生能源、同时大幅减少排放的受控系统,但由于该系统的复杂度太高,可控程度较低,其实现难度很大。高校校园可视为比较典型的城市生态系统的子系统,在合理的管控与现代信息技术的支持下,高校校园最有可能实现生态系统可控化建设。对四个主要生态流(物质流、能量流、人口流、信息流)在高校生态系统中的作用进行理论阐述,针对具有中国特色、学生大规模集中居住的高校校园,提出了一种新的受控生态系统改造方案。通过对现有校园生态工程技术进行组装,完成校园生态系统基础构筑。利用综合的校园生态系统信息流管理平台监管校园物质循环、能量流动、人口流动,探讨了可实现的高校受控生态系统的建设模式,最终提出了高校受控生态系统建设的理论模型,以期达到高校校园物质与能源利用效率最大化,降低碳排放,改善局部小型气候群,进而改善环境大气候。研究结果如能较好的应用到实践中,将为城市生态系统建设提供重要参考,意味着现代生态学将为人类发展作出一定的贡献。     

The development of a benthic ecosystem

The development of a benthic ecosystem on a sandy bottom at 3 m depth in the saline Lake Grevelingen, The Netherlands, is described. The development started after the closure of the former Grevelingen estuary and was followed for 4 1/2 years. Ecosystem attributes studied were biomass, secondary production, production/biomass ratio, type of food chains, species diversity, pattern diversity, size of organisms, type of life-cycles, and r- and K-selection. The results are discussed in relation to E. P. Odum's (1969) theory of ecosystem development. Communication nr. 150 of the Delta Institute for Hydrobiological Research     

Denitrification in a semi-arid grazing ecosystem

The effect of large herbivores on gaseous N loss from grasslands, particularly via denitrification, is poorly understood. In this study, we examined the influence of native migratory ungulates on denitrification in grasslands of Yellowstone National Park in two ways, by (1) examining the effect of artificial urine application on denitrification, and (2) comparing rates inside and outside long-term exclosures at topographically diverse locations. Artificial urine did not influence denitrification 3 and 12 days after application at hilltop, mid-slope, and slope-bottom sites. Likewise, grazers had no effect on community-level denitrification at dry exclosure sites, where rates were low. At mesic sites, however, ungulates enhanced denitrification by as much as 4 kg N ha⁻¹ year⁻¹, which was double atmospheric N inputs to this ecosystem. Denitrification enzyme activity (DEA, a measure of denitrification potential) was positively associated with soil moisture at exclosure sites, and herbivores stimulated DEA when accounting for the soil moisture effect. Glucose additons to soils increased denitrification and nitrate additions had no influence, suggesting that denitrification was limited by the amount of labile soil carbon, which previously has been shown to be enhanced by ungulates in Yellowstone. These results indicate that denitrification can be an ecologically important flux in portions of semi-arid landscapes, and that there is a previously unsuspected regulation of this process by herbivores. Received: 6 March 1998 / Accepted: 28 August 1998     

Model of a coral reef ecosystem

The results of modelling of a coral reef ecosystem at French Frigate Shoals and independent field measures of benthic primary productivity indicate relatively good agreement between food required by consumer trophic levels and organic carbon produced by primary producers. Based upon the high internal predation necessary for the model to match primary production estimates, we reason that the ecosystem is primarily regulated from the top down by forces of predation and that primary production appears to be controlled by nutrients, rate limits, and the distribution of space and habitat. In spite of relatively high primary productivity, potential yield at the top of the food chain is low because of high internal predation and high trophic complexity (6 trophic levels). Fishery yield might be maximized by harvesting low on the food chain particularly if top carnivores can be cropped to release predator pressure on selected prey. Agreement between field measures of metabolism and model (ECOPATH) results provides reasonable confidence that the model can be used as one tool for resource management.     

Denitrification in a nitrogen-limited stream ecosystem

Denitrification was measured in hyporheic, parafluvial, and bank sediments of Sycamore Creek, Arizona, a nitrogen-limited Sonoran Desert stream. We used three variations of the acetylene block technique to estimate denitrification rates, and compared these estimates to rates of nitrate production through nitrification. Subsurface sediments of Sycamore Creek are typically well-oxygenated, relatively low in nitrate, and low in organic carbon, and therefore are seemingly unlikely sites of denitrification. However, we found that denitrification potential (C & N amended, anaerobic incubations) was substantial, and even by our conservative estimates (unamended, oxic incubations and field chamber nitrous oxide accumulation), denitrification consumed 5–40% of nitrate produced by nitrification. We expected that denitrification would increase along hyporheic and parafluvial flowpaths as dissolved oxygen declined and nitrate increased. To the contrary, we found that denitrification was generally highest at the upstream ends of subsurface flowpaths where surface water had just entered the subsurface zone. This suggests that denitrifiers may be dependent on the import of surface-derived organic matter, resulting in highest denitrification rate at locations of surface-subsurface hydrologic exchange. Laboratory experiments showed that denitrification in Sycamore Creek sediments was primarily nitrogen limited and secondarily carbon limited, and was temperature dependent. Overall, the quantity of nitrate removed from the Sycamore Creek ecosystem via denitrification is significant given the nitrogen-limited status of this stream.     

Zooplankton of a swamp water ecosystem

The Great Dismal Swamp, located in southeastern Virginia and extending into northeastern North Carolina, is a unique ecosystem which has undergone severe alteration over the last 200 years due to agricultural, municipal and timbering development. The swamp is presently about 50% of its late 1700 size when George Washington commissioned the construction of the first of a series of drainage ditches that have subsequently reduced the swamp aquatic environs to a ditch network draining into Lake Drummond located near the swamp's center. The swamp waters are characterized by a brown color, high suspended organic matter, high acidity and low nutrient levels. This paper presents the first comprehensive study of the zooplankton assemblages of the Great Dismal Swamp.Zooplankton was collected for one year at 14 stations and was dominated by rotifers. Of the 84 species identified, 61 were rotifers, 18 were Cladocera and 5 were copepods. Many of the species collected were cosmopolitan and acid tolerant forms. Dominant lake rotifers included Polyarthra vulgaris, Conochiloides dossuarius, Keratella cochlearis, Trichocerca similis, Synchaeta longipes and Microcodon clavus. Dominant crustaceae included Bosmina longirostris, Diaphanosoma leuchtenbergianum, Mesocyclops edax, and Tropocyclops prasinus.Usually the ditch zooplankton was the same as that of the lake. Of the seven ditches studied, the most unique chemically and biologically were Interior, Washington, and Portsmouth. Measurable alkalinity was detected in Interior and Washington Ditches. Alkaline water rotifers such as Brachionus, Mytilina, Filinia, Notholca Platyias and Keratella earlinae were found in these ditches. The rotifer, Keratella valga, was only found from Portsmouth Ditch, during a period when water was flowing into the lake and it contained high nutrient levels.Research funded in part by the Virginia Academy of Sciences and the Center for Environmental Studies, Virginia Polytechnic Institute and State University.     

Management-driven evolution in a domesticated ecosystem

Millennia of human land-use have resulted in the widespread occurrence of what have been coined ‘domesticated ecosystems’. The anthropogenic imprints on diversity, composition, structure and functioning of such systems are well documented. However, evolutionary consequences of human activities in these ecosystems are enigmatic. Calluna vulgaris (L.) is a keystone species of coastal heathlands in northwest Europe, an ancient semi-natural landscape of considerable conservation interest. Like many species from naturally fire-prone ecosystems, Calluna shows smoke-adapted germination, but it is unclear whether this trait arose prior to the development of these semi-natural landscapes or is an evolutionary response to the anthropogenic fire regime. We show that smoke-induced germination in Calluna is found in populations from traditionally burnt coastal heathlands but is lacking in naturally occurring populations from other habitats with infrequent natural fires. Our study thus demonstrates evolutionary imprints of human land-use in semi-natural ecosystems. Evolutionary consequences of historic anthropogenic impacts on wildlife have been understudied, but understanding these consequences is necessary for informed conservation and ecosystem management.     

Seasonal shift in factors controlling net ecosystem production in a high Arctic terrestrial ecosystem

We examined factors controlling temporal changes in net ecosystem production (NEP) in a high Arctic polar semi-desert ecosystem in the snow-free season. We examined the relationships between NEP and biotic and abiotic factors in a dominant plant community (Salix polaris–moss) in the Norwegian high Arctic. Just after snowmelt in early July, the ecosystem released CO₂ into the atmosphere. A few days after snowmelt, however, the ecosystem became a CO₂ sink as the leaves of S. polaris developed. Diurnal changes in NEP mirrored changes in light incidence (photosynthetic photon flux density, PPFD) in summer. NEP was significantly correlated with PPFD when S. polaris had fully developed leaves, i.e., high photosynthetic activity. In autumn, NEP values decreased as S. polaris underwent senescence. During this time, CO₂ was sometimes released into the atmosphere. In wet conditions, moss made a larger contribution to NEP. In fact, the water content of the moss regulated NEP during autumn. Our results indicate that the main factors controlling NEP in summer are coverage and growth of S. polaris, PPFD, and precipitation. In autumn, the main factor controlling NEP is moss water content.     

Cross‐ecosystem effects of a large terrestrial herbivore on stream ecosystem functioning

Large terrestrial consumers have direct and indirect effects on forest ecosystem function, but few studies have investigated the impacts of terrestrial consumers on freshwater ecosystems. In the Cape Breton Highlands of Nova Scotia, browsing by hyper‐abundant moose following a spruce budworm outbreak has transformed boreal forest into grasslands. We conducted a field study to investigate the potential for cross‐ecosystem effects of hyper‐abundant moose following budworm outbreak on small boreal stream ecosystem structure and function. With our field study, we tested the prediction that watersheds with higher levels of moose‐mediated grasslands in their sub‐basin would have higher stream temperatures, total nitrogen, electrical conductivity, periphyton biomass and macroinvertebrate abundances. While our data supported several of our predictions pertaining to moose impacts on the abiotic variables (i.e. temperature range, total nitrogen, electrical conductivity) we found evidence of variable moose impacts on the benthic community. Specifically, we observed lower relative abundance of predatory invertebrates in streams with high moose impacts compared to streams with low moose impacts in their watersheds but no evidence of moose impacts on the relative abundance of shredders, filterers, gatherers, and grazers. This empirical study fills a key gap in our understanding of spatial ecosystem ecology by providing insight into the effects of large terrestrial consumers across ecosystem boundaries with potential implications for landscape‐scale management of hyper‐abundant ungulates. Given the broad availability and improvement in remote sensing technology, the novel integration of remote sensing and field studies employed here may provide a roadmap for future studies of meta‐ecosystem dynamics.     

Nitrogen budget of a shortgrass prairie ecosystem

Summary A N budget is presented for a shortgrass prairie ecosystem. The grassland was ungrazed by domestic herbivores. The quantities of N in various plant, animal, microorganism, and soil components of the ecosystem are estimated for the date when aboveground living biomass was at its maximum for the growing season of 1973. Annual transfers of N between the various compartments were also estimated.Of the total N, 99.5% was in organic forms. The relatively inert heteropolycondensate fraction of the organic matter in the soils contained 88.8% of the N. Living organisms contained 4.2% and dead but recognizable organisms or part thereof contained 6.5% of the total N. Belowground animals contained more than 10 times as much N as abovegroud animals, but combined, animals contained less than 0.1% of the total in the system. Living plant material contained 2.5% of the total N. Seventy-two percent of the living plant N was below ground. Microorganisms contained 1.4% of the total N.Total N uptake by plants from soil solution was 2.9 g·m^-2·yr^-1. Aerial portions of plants were allocated 1.9 N·m^-2·yr^-1 although apparently 26% of this amount came from internally recycled sources. The heteropolycondensate fraction of the soil contributed 0.7 g N·m^-2·yr^-1 to mineral forms, but these components of the system were assumed to be in steady state; thus an equal amount of mineral N was allocated back to the source. Mineralization of N from plant residues was sufficient to account for all of the N taken up by plants from soil solution. Soil animals immobilized about 0.4 g N·m^-2·yr^-1 while the amount shunted to aboveground animals was trivial.     

Stochastic simulations of a synthetic bacteria-yeast ecosystem

ABSTRACT: BACKGROUND: The eld of synthetic biology has greatly evolved and numerous functions can now be implemented by articially engineered cells carrying the appropriate genetic information. However, in order for the cells to robustly perform complex or multiple tasks, co-operation between them may be necessary. Therefore, various synthetic biological systems whose functionality requires cell-cell communication are being designed. These systems, microbial consortia, are composed of engineered cells and exhibit a wide range of behaviors. These include yeast cells whose growth is dependent on one another, or bacteria that kill or rescue each other, synchronize, behave as predator-prey ecosystems or invade cancer cells. RESULTS: In this paper, we study a synthetic ecosystem comprising of bacteria and yeast that communicate with and benet from each other using small diffusible molecules. We explore the behavior of this heterogeneous microbial consortium, composed of Saccharomyces cerevisiae and Escherichia coli cells, using stochastic modeling. The stochastic model captures the relevant intra-cellular and inter-cellular interactions taking place in and between the eukaryotic and prokaryotic cells. Integration of well-characterized molecular regulatory elements into these two microbes allows for communication through quorum sensing. A gene controlling growth in yeast is induced by bacteria via chemical signals and vice versa. Interesting dynamics that are common in natural ecosystems, such as obligatory and facultative mutualism, extinction, commensalism and predator-prey like dynamics are observed. We investigate and report on the conditions under which the two species can successfully communicate and rescue each other. CONCLUSIONS: This study explores the various behaviors exhibited by the cohabitation of engineered yeast and bacterial cells. The way that the model is built allows for studying the dynamics of any system consisting of two species communicating with one another via chemical signals. Therefore, key information acquired by our model may potentially drive the experimental design of various synthetic heterogeneous ecosystems.     

Nitrogen fixation in a desert stream ecosystem

Few measurements of nitrogen fixation exist for streams. Desertstreams are warm, well lighted, and often supportabundant cyanobacterial populations; thus N₂ fixationmay be significant in these N-poor ecosystems. N₂fixation was measured in situ by acetylene reductionfor two patch types (Anabaena mat and anepilithic assemblage). Patch-specific rates were highcompared with published values (maximum 775 µgN₂ [83 µmol C₂H₄]mg chl a ^-1 h^-1or 51 mg N₂ [5.4 mmol C₂H₄] m_-2 h_-1).Daytime fixation was higher than nighttimefixation, and temperature, light and inorganic Nconcentration explained 52% of variance in hourlyrates over all dates. Diel input-output budgets wereconstructed on five dates when cyanobacteria werepresent in the stream. Diel N₂ fixation rates weremeasured for comparison with reach-scale diel nitrogenretention, to assess the importance of this vector to Neconomy of the stream. Fixation accounted for up to85% of net N flux to the benthos, but its importancevaried seasonally. Finally, we applied biomass-specificfixation rates to 1992 and 1993 biomass data to obtainseasonal and annual N₂ fixation estimates.Cyanobacteria were absent or rare during winter andspring, thus most of the annual N₂ fixation occurredduring summer and autumn. Annual rates of nitrogenfixation for 1992 and 1993 (8.0 g/m₂ and 12.5g/m₂) were very high compared to other streams,and moderately high compared to other ecosystems.Like other phenomena in this disturbance-proneecosystem, nitrogen fixation is strongly influenced bythe number and temporal distribution of flood events.     

A model of a digital biological ecosystem

In this paper, we propose a model of a digital biological ecosystem of fish. Collections of fish data by scientists in Malaysia have been converted and developed into a digital biological ecosystem using computational technology and methods. We used a combination of Geographical Information System, databases and ontologies for storing, retrieving and visualizing fish species distribution and their abundance as well as their relationship with the environment. We used ArcGIS to build the fish and environmental geodatabase, which is linked to Google Earth for real-time visualization, and Surfer 8 to create contour maps which are superimposed as layers on the ArcGIS interface. Individual fish species on the map are hyperlinked to the FishBase Portal (http://www.fishbase.org/) while the published map is displayed using ArcReader. The three databases that we created contain information about fish species, environment and contours. These are also integrated using a fish ontology which will link all the available information for various fish species. The proposed system can be adopted by marine scientists to better convince economists, fishery managers, coastal developers and government bodies who make important decisions on conservation policies and laws.     

Marine plants in a coral reef ecosystem

Based on a review of the literature and our own data, marine plants are shown to play an important role in the formation and sustaining of coral reefs, which are one of coastal tropical ecosystems of the World Ocean. The important ecosystem roles of marine plants include primary production and recycling of organic matter, the construction of the hard base of a coral reef, the fixation of dissolved molecular nitrogen in sea-water, the formation of an initial link in the food chain, the provision of a habitat for marine animals, and the protection of the reef against destructive wave action.