General water chemistry and quality in newly-created subtropical wetland lake

Sixty km2 of the southern Hula Valley (northern Israel) peat lands were flooded in 1994 as part of the Hula Valley Restoration Project. The small, shallow lake (110 ha, mean depth < 1 m) and network of ca. 90 km of canals created were designed to ameliorate problems (e.g., underground fires, soil subsidence, increased nutrient loading downstream to Lake Kinneret) resulting from drying the Lake Hula wetlands in the 1950s. This new wetland area now serves as the focus for developing eco-tourism in northern Israel. The initial development of this new ecosystem has been followed closely by a multi-disciplinary team of researchers, with an emphasis on water quality in the new lake and the potential impact of the project on Lake Kinneret. Here we report an overview of developments in general water chemistry of Lake Agmon during its first three years (1994–1996). Water quality in Agmon was within general expectations for a shallow lake situated on peat. The first year of Agmon was characterized by the heavy influence of stream and drainage inflows with high pH, alkalinity, turbidity and electrical conductivity and high concentrations of sulfate and total dissolved solids. By the third year, however, many in lake processes (e.g., nutrient cycling and algal and macrophytic production) were well-developed and thus strongly affected lake water quality. Excessive phosphorus and nitrogen concentrations in the lake have led to hypertrophy, characterized by low dissolved oxygen concentrations and prolific blooms of nuisance algae. The management of this new ecosystem in the near future will require persistent, and innovative measures.     

Repopulation and colonization by birds in the Agmon Wetland,Israel

Lake Hula and its surrounding wetland in northern Israel were drained in the late 1950s and the dried wetlands were transformed into a diverse agricultural region with a 0.3 km2 nature reserve. A portion of the extinct Hula wetland was re-flooded in April 1994 by constructing a small lake, Agmon, and 90 km of canals. The purposes of this study were (a) to document the re-population and colonization of the new Agmon wetland by birds after its flooding, (b) to evaluate bird species richness in this new wetland in comparison to that in a nearby mature Hula Nature Reserve, and, (c) to investigate if the species originally present in the Hula Valley before the drainage had been re-established. The new lake has succeeded in attracting a large variety of water birds to the newly formed habitats, especially ducks, egrets and herons, plovers, waders and snipes. The distribution of bird species among the different habitats was not random. The northern section of the lake, which is shallow and has an open shore, had the largest number of species during 1995 and 1996 and was preferred by plovers, waders and snipes. A large roosting and breeding colony of thousands of egrets and herons was formed in the dense cattails ( Typha domingensis) in the southern section of the lake. Unlike the nearby Hula Nature Reserve, the new wetland lacks a large seasonally flooded area and is less attractive for feeding and breeding plovers, waders and stilts. The new wetland also has very little muddy area without vegetation and attracts few of the species that regularly feed in this habitat in the reserve. The new wetland enlarges the area of only a few of the habitats found in the nearby reserve and therefore attracts fewer species than it might otherwise. Recommendations for management of the new wetland include increased diversity of habitats, restriction of human activities and optimization of conflicts that have arisen between the needs of the wetland and those of nearby agriculture.     

Phytoplankton-metaphyton seasonal dynamics in a newly-created subtropical wetland lake

The dynamics of the algal populations of Lake Agmon, a newly created shallow lake in the Hula Valley, Israel, were monitored following its filling in April 1994 through 1996. Additional limited field observations and measurements were taken throughout 1997. Following an initial establishment period, the dynamics of the algal populations showed a repetitive annual pattern comprised of three phases: I. a clear water phase in January–February, with low phytoplankton biomass and no metaphyton; II. a metaphyton dominance phase during March–June when mats of filamentous chlorophytes covered most of the lake's sediments while phytoplankton biomass remained low; and III. an intense phytoplankton bloom phase from June till December. The shifts from phase I to II and from phase II to III were gradual, resulting from interplay between phosphorus availability, the underwater light climate, temperature effects and zooplankton grazing pressure. The shift from phase III back to phase I was abrupt, due to winter flushing of Lake Agmon. The summer phytoplankton blooms intensified from 1994 to 1996 and shifted from chlorophyte dominance in 1994 and 1995 to cyanobacteria-dominance in 1996 and 1997. These observations, jointly with the nutrient chemistry of Lake Agmon, suggest intense eutrophication. Criteria based on phytoplankton taxonomy also indicate that Lake Agmon is eutrophic to hypertrophic. Due to the typical unstable nature of hypertrophic systems, careful management is essential to maintain the delicate ecological balance needed to ensure that the lake will fulfill its intended role as a center for eco-tourism.     

Temporal variation in fish community structure in a newly created wetland lake (Lake Agmon) in Israel

Lake Agmon was constructed in summer 1994 in the northern part of the drained Lake Hula swamp, as part of the Hula Reclamation Project. One of the main goals of the project was to attract aquatic and semi- aquatic birds to the area as a basis for planned eco-tourism and one of the main concerns of the project was the potential for increased proliferation of mosquitoes (including vector species of malarial parasites). There was a perceived need, therefore, to establish and maintain a suitable fish community. This present study documents the developments in the fish community in Lake Agmon between May 1995 and December 1996. The lake was initially stocked with two fish species, Tilapia zillii and Gambusia affinis, to control mosquitoes and to provide suitable small- bodied forage species for piscivorous birds. Subsequent stocking also included Oreochromis aureus, and Cyprinus carpio. Additional species were established by immigration from the Jordan River. Relatively large species ( e.g., Clarias gariepinus and C. carpio) flowed into the lake as eggs or juveniles, whereas the smaller species ( e.g., Hemigrammocapoeta nana, Pseudophoxinus kervillei and Aphanius mento) entered the lake as adults. In the first year, eight fish species were found in Lake Agmon: T. zillii, G. affinis, C. gariepinus, C. carpio, Capoeta damascina, P. kervillei, Acanthobrama lissneri and H. nana. Of these, T. zillii, G. affinis and H. nana were dominant, though the relative abundance of H. nana was very low in spring, and increased during summer. In the second year, O. aureus, A. mento and Anguilla anguilla also occurred in the lake. The density of P. kervillei increased, in comparison with the previous year. The relative proportions of juvenile and adult fish also changed in the second year. A high percentage of young T. zillii was found during the first spring, decreasing in the summer and autumn. The proportion of juveniles of both G. affinnis and H. nana was very low during the first year, but increased during the second. These results indicate that the fish community of Lake Agmon had not stabilized by the end of 1996 and that further changes in relative abundances, and species, age and sex compositions should be expected.     

Nutrient and plant dynamics in Lake Agmon Wetlands (Hula Valley,Israel): a review with emphasis on Typha domingensis (1994–1999)

Shallow lake Agmon is a newly created subtropical wetland in north-eastern Israel. The lake is part of the Hula Project aimed at slowing down deterioration processes of the peat soils, to establish infrastructure for ecotourism as an income for the land owners, and nutrient removal from Lake Kinneret inputs. An onset of benthic filamentous macro-green algae during late winter–spring season, followed by submerged macrophytes vegetation during spring–summer was documented. The phosphorus summer loads are mostly plant–mediated internal fluxes and nitrogen intensively removed from lake waters by sedimentation and denitrification. The summer phytoplankton, mostly colonial cyanobacteria, are P limited. During 1995 and early 1996, dense Typha domingensisstands were developed in the southern half of the Lake (chalk-marl bottom sediments). The P-limited Typhavegetation collapsed within less than half a year and reappeared in the south-eastern part of the lake where sediments were exposed and oxidized. It is hypothesized that phosphorus cycle is a strong dependant of macrophyte mediation, and P deficiency in the sediments predominantly affected Typhadecline and an increase of P availability later enabled the reappearance of the Typhastands.     

Cyclopoid diversity in the basin of Lake Hula (Israel), after its partial reflooding

In a relatively small area of 60 km² which corresponds to the basin of the presently drained Lake Hula and its swamps (Upper Jordan Valley), 22 species of Cyclopoida are on record, with two more species reported in the pre-drainage times. The basin of Lake Hula is the southernmost enclave of permanent fresh waters in the Levant Province of Southwest Asia. Lacustrine and swamp environments existed in the area uninterruptedly for at least 700 000 years. A partial restoration project created a new lake. The basin is situated right in the middle of a main bird migration route. The fact that no less than 15 species were recorded from a set of small artificial and isolated experimental ponds seems to indicate that migrating birds and stocks of resting eggs are to account for this high diversity. Cyclops vicinus, Mesocyclops arcanus and Eucyclops serrulatus are the most common species. The success of the restoration is discussed.     

Foraging,roosting, and nesting habitats of the avian fauna of the Agmon wetland,northern Israel

The foraging, nesting and roosting habitats of the avian fauna of a newly created Agmon wetland and surrounding cultivated peat land (5 km2) in the Hula Valley, northern Israel, were evaluated (January 1996–February 1997) to assess the value as a habitat and for wildlife tourism. We recorded 180 bird species (herons, dabbling ducks, kingfishers, waders, wagtails and raptors) in different habitats (the lake, shores, cattail and reed-bed stands, trees, temporary inundated areas). The most heavily used habitat for foraging, breeding, and roosting was a large cattail stand in the southern third of the lake. The foraging habitat and diet data of 97 avian species were determined. The most intensively used foraging habitats were cultivated fields, lake shore reed-beds, shallow canals and the cattail stand. Forty six species nested in the wetland during March-October, with 2,040 colonial and solitary nests mostly in the cattail stand, near-shore reed-beds and young trees. Roosts, also mostly in the cattail and reed-bed stands and in trees, were used by 55 species. Based on this survey of available habitats, we identified several key habitats that are either missing or require further development (e.g., temporarily inundated mud flats, reed-beds and bare islands). We also provide suggestions for improving the delicate balance between requirements of this developing wetland ecosystem and of the adjacent agricultural areas.     

Development of macrophytic vegetation in the Agmon Wetland of Israel by spontaneous colonization and reintroduction

The draining of the Lake Hula and swamps, northern Israel, during the late 1950s resulted in the loss of a very diverse and rare ecosystem. Oxidation of the peat soil resulted in ground surface subsidence, while heavy autumn winds have eroded the dry peat. Moreover, agriculture on the peat soils is restricted, because of a nitrate surplus. Predictions that the sinking would continue and that more areas would go out of agricultural production led authorities to re-flood a portion of the Hula Valley in 1994. The aim of the present study was to monitor the spontaneous establishment of vegetation in the re-flooded area, the Agmon wetlands, and to reestablish some of the major plant species lost from the valley when Lake Hula was drained. Within the first two years, 74 plant species colonized the wetland spontaneously. Five out of 11 species designated for reintroduction were successfully established. Cyperus papyrus and Cynodon dactylon demonstrated sustainable potential for lake-shore stabilization. Cyperus papyrus was reintroduced from seedlings and rapidly became the dominant riparian species, while Cynodon dactylon established spontaneously. Re-introduced Nymphaea alba clones were established only in enclosures protected from grazing by the semi-aquatic mammal Myocastor coypu. Nuphar lutea and Iris pseudacorus showed better resistance to grazing. These results demonstrate a high potential for successful re-establishment of much of the original Hula swamp macrophytic vegetation by either spontaneous colonization by extant species from the surrounding areas or by introduction of locally extinct species. As such, there is a good chance that the associated faunal components of the former Lake Hula and swamps that have returned to the region since the Hula rehabilitation project commenced will continue to flourish.     

Abstracts

Lake Agmon was created in the Hula Valley in Israel, in the northern part of the dried-up Hula Lake site, in summer, 1994. Samples of fish at ten stations were taken by electroshocker once a month, from January to December, 1996. The fish species whose food composition in the gut was examined in this study were: Tilapia zillii, Gambusia affinis, Clarias gariepinus, Cyprinus carpio, Pseudophoxinus kervillei, Acanthobrama lissneri, Hemigrammocapoeta nana and Oreochromis aureus. Food components were determined qualitatively and quantitatively. Assessment of the organism biomass in the gut contents was based on available data of phytoplankton and zooplankton. The food of G. affinis changed during the year, consisting high level of algae in winter and spring, and insects and crustaceans in summer. In T. zillii, a high percentage of algae were found in winter, and a high percentage of plants in summer. The food of H. nana consisted mainly of phytoplankton, but included high plants during most months; P. kervillei ingested mainly insects and crustaceans, with a high percentage of Daphnia spp.; and the diet of C. gariepinus comprised fish and invertebrates species, which varied with the seasons. C. carpio ate mainly invertebrates; O. aureus are vegetarian, and A. lissneri fed on both animals and plants. This revised version was published online in July 2006 with corrections to the Cover Date.     

Strontium isotopes in Melanopsis sp. as indicators of variation in hydrology and climate in the Upper Jordan Valley during the Early-Middle Pleistocene, and wider implications

Aquifers dominated by Pleistocene basalts and Jurassic to Cretaceous calcareous rocks feed the Hula basin which is drained by the Jordan River into Lake Kinneret. The sedimentary sequence of Lower-Middle Pleistocene Benot Ya‘akov Formation (BYF) exposed by excavations of the 0.78 Ma lake-side site of Gesher Benot Ya‘aqov (GBY) consists of six cycles representing ca. 100 ka history of the Hula basin. This study characterizes the types of water sources in the catchment, tests the use of the Strontium (Sr) isotopes in the common extant snail Melanopsis sp. as a tracer for water in its habitat, and uses this tracer in the fossil specimens from GBY to investigate the palaeohydrology of the Hula paleolake during the corresponding period.The Sr isotope composition (⁸⁷Sr/⁸⁶Sr) of extant Melanopsis shells in the Hula catchment range widely (0.7046-0.7079). These analyses define distinct groups of water sources and aquifers, while the Jordan River at the GBY site has values around 0.70685. The values for fossil Melanopsis from GBY vary along stratigraphy; they are highest around 0.70710 in Cycles 1 and 2, decrease to around 0.70685 in Cycle 3, and exhibit upward trending fluctuations in the subsequent cycles to 0.70703 in Cycle 6. This trend reveals the dominance of the Hermon Jurassic aquifer during the earlier, colder periods before the Matuyama-Brunhes Boundary (MBB) and enhanced influence of the Golan basaltic aquifers, in subsequent warmer periods, indicating that the MBB coincides with climate warming as supported by other indicators. Hence, this global geochronological indicator of 0.78 Ma is also potentially a global palaeoclimatic marker. The similarity between the Sr isotope composition of the Jordan River waters and Melanopsis and those from Cycle 3 suggests that the current climate corresponds to that of the warmest period within the record of GBY, clarifying the comparative interpretation of this 100 k.yr. climate record.     

Biogeochemical evolution of a sulfur-iron rich aquatic system in a reflooded wetland environment (Lake Agmon,northern Israel)

Major biogeochemical processes in the newly created, shallow Lake Agmon (Hula Valley, northern Israel) were investigated from 1994 to 1996. Sediment cores, lake water and porewater were analyzed for chemical composition and spatial distribution. Sediment analyses revealed that Lake Agmon has two different sediment types: peat sediments in the northern and central parts, and marls in the southern part. The basic composition of the lake's water was controlled mainly by the mixing of two distinct water types (Jordan River and water drainage), and by evaporation. About 3/4 of the lake water originated from the Jordan Inlet, a quarter through the Z Canal Inlet (peat drainage) and a minor amount from groundwater seepage. Lake Agmon is unique among freshwater wetlands owing to its high SO ₄ ^2– content, which is ca. 1/3 that of sea water. This characteristic is ascribed to the dissolution of secondary gypsum, formed in the peat soils since the drainage of the historic Hula Marsh. Leaching gypsum from the shallow sediments during the first few months after flooding was followed by a later stage of constant diffusion and advection of SO ₄ ^2– from gypsum dissolution in deeper sediments. Gypsum dissolution in lake sediments contributed ca. half of the SO₄ ^2– and Ca²⁺ inputs to the lake. The concomitant increase of Ca²⁺ combined with alkalinity release due to organic matter decomposition in the sediments led to the precipitation of CaCO₃. This precipitation was enhanced by photosynthesis, particularly during summers, and consumed about a tenth of the Ca²⁺ and third of the alkalinity outputs from the lake. Iron-hydroxide was the main agent for microbial oxidation of organic matter, surpassing by far the role of sulfate, nitrate and manganese as electron acceptors. The produced Fe²⁺ was transported upward by diffusion and advection and oxidized to ferric iron at the sediment-water interface. There is evidence, however, that some sulfate was reduced, but most of the produced sulfide reacted with ferrous iron and accumulated in the sediments as FeS minerals. Therefore, despite high sulfate concentrations, the high iron availability restricted release of toxic sulfides into the water and thereby served to maintain reasonable water quality.     

A palynological study of the Acheulian site of Gesher Benot Ya’aqov, Israel

The results are discussed of the palynological (pollen-analytical) examination of a sediment section in the Hula Valley of northern Israel, with evidence of Acheulian occupation dated to 700,000–800,000 b.p. In general there is a fair agreement between the palynological data and the wood remains identified from the site, but there are also discrepancies, some of which can be explained and others not. Although relatively well represented in the pollen record, Pinus (pine) most probably did not occur in the Hula area. Some pollen types are thought to have been carried in from hundreds of kilometres away (long-distance transport). Together the pollen and wood evidence suggests that Quercus ithaburensis–Pistacia atlantica (Tabor oak–Atlantic terebinth) woodland (open forest) was found in the Hula Valley (other than the lake and marshes) and on the lower reaches of the mountains flanking the valley on both sides. In addition to deciduous Tabor oak, evergreen Kermes oak (Quercus calliprinos) must have been an important component of this woodland. Wild olive (Olea europaea var. oleaster) may also have been quite common here. The suggestion of open forest, with fairly widely spaced trees, is based upon the high non-arboreal pollen frequencies and indicates fairly dry climatic conditions. Various stream-bank trees and shrubs are represented in the pollen and/or wood records, such as Fraxinus (ash), Ulmus (elm), Salix (willow) and Platanus (plane tree). During the period represented by the upper section of the pollen diagram, Cedrus (cedar) must have reached the Hula area, indicating increased humidity. In the steppe-like field layer (undergrowth of the woodland) grasses (Gramineae) must have played a prominent role in addition to a great number of other species. In particular Compositae and Umbelliferae include a large variety of species (many different pollen types). Two Chenopodiaceae maxima, coinciding with Gramineae minima, are thought to be indicative of periods of increased climatic dryness. The local lake and marsh vegetation is fairly well represented in the pollen record, but interpretation in terms of vegetation succession is only possible to some degree. Mention is made here of Trapa natans (water chestnut), the nuts of which were consumed by the Acheulian inhabitants. Sytze Bottema: Deceased in 2005.     

云南石林长湖湿地植物区系研究

论述云南石林县长湖湖泊湿地范围内湿地植物的植物区系组成及地理成分特点,为保护和利用湿地资源提供科学依据。结果表明:(1)有湿地植物20科47属56种,种类多样性较突出;(2)植物区系统计,广布的科、属、种分别占95%、40.4%、19.6%,湿地植物的广布性突出;(3)科级区系中热带分布占5%,属级区系中热带分布占38.2%、温带分布占21.4%,种级区系中热带分布占32.2%、温带分布占42.8%,属级和种级区系显示亚热带区系的区域性;(4)种级区系中特有分布占5.4%,且为当地特有变种,显示出较高特有性。     

大型浅水湖泊鄱阳湖湿地微生物的研究现状

鄱阳湖是我国第一大淡水湖泊,同时也是一个典型的季节性通江浅水湖泊,独特的水文特征和多样的湿地景观类型形成了复杂多样的微生物群落。本文综述了鄱阳湖水文节律、营养盐及重金属含量对湖泊微生物群落组成的影响,以及水位高程和湿地围垦对鄱阳湖湿地土壤微生物分布特征的影响,同时还探讨了未来湖泊湿地微生物的研究方向和鄱阳湖所拥有的独特研究条件,以期为未来湖泊微生物研究提供重要参考。     

Present–absent: a chronicle of the dinoflagellate Peridinium gatunense from Lake Kinneret

A long-term record dating back to the 1960s indicates that Peridinium gatunense, an armored dinoflagellate, dominated the phytoplankton of Lake Kinneret (Sea of Galilee, Israel) until the mid-1990s, with a relatively stable spring bloom. However, since 1996, these blooms became irregular, failing to develop in 10 out of the past 16 years. During the later period, a significant correlation (R ² = 0.605, P = 0.013) was found between annual peak P. gatunense biomass and riverine inflow volume. In-lake surveys showed that patches of high P. gatunense densities were associated with water enriched with fresher inflowing Jordan River water. Supplementing laboratory cultures of P. gatunense with Hula Valley water stimulated its growth relative to un-enriched controls. A likely explanation to the recent irregular blooms of this dinoflagellate is a hydrological modification that was made in the catchment in the mid-1990s, preventing Hula Valley water from reaching Lake Kinneret in most years—except for exceptionally wet years. We propose that until the mid-1990s, the Jordan River water enriched Lake Kinneret with a growth factor (a microelement and/or organic compound) originating in the Hula Valley, which in recent years has arrived in sufficient quantities to support a bloom only in high-rainfall years.     

人工和天然湿地芦苇根际土壤细菌群落结构多样性的比较

为认识人工湿地运行初期根际土壤细菌群落的结构多样性,本研究采用聚合酶链式反应-变性梯度凝胶电泳（PCR-DGGE）的方法,比较了嘉兴石臼漾人工构筑生态湿地和白洋淀天然湿地府河河口区域芦苇根际土壤的细菌群落结构多样性。研究结果显示,嘉兴石臼漾湿地在运行初期（1~1.5年）,根际土壤细菌的物种丰富度已与白洋淀湿地相近,但香农指数和均匀度指数均显著低于白洋淀湿地;随着污染物浓度的降低,土壤细菌群落基因型多样性指数增大。     

抚仙湖窑泥沟人工湿地的除磷效果研究

为了减缓和控制抚仙湖局部湖湾水体富营养化趋势,在抚仙湖北岸建设了净化面积1 hm²的人工湿地.综合利用生物氧化塘、水平潜流人工湿地和表面流人工湿地治理技术,对入湖河道窑泥沟污水中磷的去除效果进行了试验研究.结果表明,该人工湿地系统对磷具有较强的去除能力.总磷去除率在57.7%～81.10%之间,平均去除率为54.9%.单位面积磷滞留量平均为26 mg·m^-2·d^-1,其中,湿地植物同化作用磷滞留量为26.1 mg·m^-2·d^-1,约占磷滞留总量的10%,大部分磷去除是通过基质吸附和沉降作用,但主要湿地植物水芹的季节变化对相应功能区的除磷效果会产生一定影响.试验期间,各功能区单位面积磷滞留量依次为水平潜流人工湿地＞生物氧化塘＞沉淀池＞表面流人工湿地.     

异龙湖湿地修复后可培养酵母菌的多样性及其与理化因子的相关性

【目的】研究湿地修复后异龙湖中可培养酵母菌多样性及其与理化因子的相关性。【方法】对异龙湖湖水中可培养酵母菌进行DNA提取和测序,通过分析26SrRNA基因的D1/D2区域和形态以及生理生化特征对酵母菌进行鉴定,测定各个水样点的总有机碳(TOC)、总氮(TN)、总磷(TP)、总硬度(TH)和电导率(Cond),运用R 4.0.5、Canoco 5软件来分析异龙湖湖水中可培养酵母菌多样性和与理化因子的相关性。【结果】从湿地修复后的异龙湖湖水中分离获得519株可培养酵母菌,鉴定为24个属42个种和1个潜在的新种,胶红酵母(Rhodotorula mucilaginosa)、皮肤皮状新丝孢酵母(Cutaneotrichosporon dermatis)以及产黑色素短梗霉(Aureobasidium melanogenum)是异龙湖中的优势种,分别分离到了320株(52.29%)、40株(7.71%)和37株(7.13%)。【结论】湿地修复后的异龙湖具有丰富的可培养酵母菌资源,其群落结构较湿地修复前有了明显的变化,湖区西北部的可培养酵母菌多样性要比湖区东南部丰富。TN与异龙湖中可培养酵母菌多样性...     

Extinction of water plants in the Hula Valley: Evidence for climate change

We describe two events of water plant extinction in the Hula Valley, northern Israel: the ancient, natural extinction of 3 out of 14 extinct species at Gesher Benot Ya‘aqov, which occurred some 800-700 k.yr., and an anthropogenic, near contemporary extinction of seven species in the artificial drainage of the Hula Lake in the 1950s. We conclude that the considerable fraction of water plants that disappeared from the Hula Valley in the Early-Middle Pleistocene was the result of habitat desiccation and not global warming. Thus, there is evidence that the hominins who lived in the Hula Valley inhabited a comparatively dry place. The disappearance of water plant species was partially the result of reduced seed dispersal by birds (ornitochory) as a result of the shrinkage of water bodies and their number along the Rift Valley. We suggest that the disappearance of a group of rare, local water plants can be used as an indicator of climate drying and impacts on the local vegetation.