Distributional patterns of freshwater taxa (fishes, crustaceans and plants) from the Mexican Transition Zone

Aim  To test whether distributional patterns of Neotropical freshwater taxa fit the generalized tracks already postulated for terrestrial groups occurring in the Mexican Transition Zone.
Location  The study units comprised 17 hydrological basins located along the Pacific coast of the Americas from Mexico to Panama, and in the Gulf of Mexico from the Papaloapan to the Grijalva–Usumacinta basin.
Methods  Distributional data for 22 fish species, 34 crab species of the tribe Pseudothelphusini, and 22 strictly freshwater species of angiosperms were analysed. Parsimony analysis of endemicity is based on presence/absence data of these taxa and uses the computer programs Winclada and NONA.
Results  Three generalized tracks were obtained: (1) Mexican North Pacific, (2) Mexican Central Pacific, and (3) Southern Mexico–Guatemala. A node resulted at the intersection of the first two tracks, coinciding with the Neovolcanic Axis in central Mexico.
Main conclusions  Freshwater generalized tracks with an altitudinal distribution below 1000 m, mainly including fishes and angiosperms, are close to the Tropical Mesoamerican generalized track. Generalized tracks above 1000 m, including freshwater crabs, have a stronger affinity with the Mountain Mesoamerican track. The Isthmus of Tehuantepec represents a node for the Neotropical freshwater and terrestrial biota. These results seem to indicate that common geobiotic processes have induced these patterns.     

The impact of ski slopes management on Krvavec ski resort (Slovenia) on hydrological functions of soils

The study was performed on the ski resort Krvavec, which is one of the most frequented ski resorts in Slovenia. The ski slopes serve as pastures for cattle during summer time and range from 1500 to 2000 m a.s.l., which is at or above the upper timberline. To offer a longer ski season and to profit snow better (either natural or artificial one) the slopes have been levelled and consequently the soil profile has been changed. Such altered soil profile characteristics strongly impact hydrological functions of soils. To study these impacts, five plots (20 × 20 m) have been chosen on the slopes with a different history: pasture without any amelioration work, a patch of forest in the ski resort without any ameliorations, and three plots with different intensity of amelioration. Dynamics of soil water content on each plot has been determined by measuring soil water content in-situ with portable TDR system during several days after long lasting heavy rains. Statistically significant differences were shown in soil water content between the plots after the rain, although some differences between plots have disappeared in the following days.     

Decadal change in wetland–woodland boundaries during the late 20th century reflects climatic trends

Wetlands are important and restricted habitats for dependent biota and play vital roles in landscape function, hydrology and carbon sequestration. They are also likely to be one of the most sensitive components of the terrestrial biosphere to global climate change. An understanding of relationships between wetland persistence and climate is imperative for predicting, mitigating and adapting to the impacts of future climate change on wetland extent and function. We investigated whether mire wetlands had contracted, expanded or remained stable during 1960–2000. We chose a study area encompassing a regional climatic gradient in southeastern Australia, specifically to avoid confounding effects of water extraction on wetland hydrology and extent. We first characterized trends in climate by examining data from local weather stations, which showed a slight increase in precipitation and marked decline in pan evaporation over the relevant period. Remote sensing of vegetation boundaries showed a marked lateral expansion of mires during 1961–1998, and a corresponding contraction of woodland. The spatial patterns in vegetation change were consistent with the regional climatic gradient and showed a weaker co‐relationship to fire history. Resource exploitation, wildland fires and autogenic mire development failed to explain the observed expansion of mire vegetation in the absence of climate change. We therefore conclude that the extent of mire wetlands is likely to be sensitive to variation in climatic moisture over decadal time scales. Late 20th‐century trends in climatic moisture may be related primarily to reduced irradiance and/or reduced wind speeds. In the 21st century, however, net climatic moisture in this region is projected to decline. As mires are apparently sensitive to hydrological change, we anticipate lateral contraction of mire boundaries in coming decades as projected climatic drying eventuates. This raises concerns about the future hydrological functions, carbon storage capacity and unique biodiversity of these important ecosystems.     

Patterns and Pathways in the Post-Establishment Spread of Non-Indigenous Aquatic Species: The Slowing Invasion of North American Inland Lakes by the Zebra Mussel

The zebra mussel, Dreissena polymorpha, has spread through eastern North American aquatic ecosystems during the past 15 years. Whereas spread among navigable waterways was rapid, the invasion of isolated watersheds has progressed more slowly and less predictably. We examined the patterns of overland spread over multiple spatial and temporal extents including individual lake districts, states, and multi-state regions in the USA and found that only a small proportion (<8%) of suitable inland lakes have been invaded, with the rate of invasion appearing to be slowing. Of the 293 lakes known to be invaded, 97% are located in states adjacent to the Laurentian Great Lakes with over half located in Michigan. Only six states have more than 10 invaded lakes and only in Michigan and Indiana have more than 10% of suitable lakes become invaded. At smaller spatial extents, invaded lakes are often clustered within a lake-rich region across southern Michigan and northern Indiana. This clustering appears primarily due to multiple overland invasions originating from the Great Lakes followed to a lesser extent by subsequent secondary overland and downstream dispersal. Downstream spread appears responsible for only one third of the inland invasions. Temporally, invasions peaked in the late 1990s, with only 13 new invasions (0.4% of suitable lakes) reported in 2003 in the four-state region surrounding Lake Michigan. Peak rates of invasion occurred 4–6 years earlier in Michigan relative to Indiana and Wisconsin, but this time lag is likely due to differences in the establishment of Great Lake source populations rather than ‘stepping stone’ dispersal across the landscape.     

Toward a plant-based proxy for the isotope ratio of atmospheric water vapor

Atmospheric water vapor is a major component of the global hydrological cycle, but the isotopic balance of vapor is largely unknown. Here, using models and observations, we show that the leaf water δ¹⁸O in the tropical Crassulacean acid metabolism (CAM) epiphyte Tillandsia usneoides is controlled by the δ¹⁸O of atmospheric water vapor in a predictable manner, irrespective of precipitation inputs. By taking the leaf‐water‐atmospheric signature as recorded in plant organic material, we have reconstructed the atmospheric water vapor δ¹⁸O signature for Miami, FL, USA between 1878 and 2005 using contemporary and herbarium specimens. T. usneoides ranges from Virginia, USA southwards through the tropics to Argentina, and the CAM epiphytic lifeform is widespread in other species. Therefore, there is significant potential for using epiphytes to reconstruct the isotope ratio of atmospheric water (both δ¹⁸O and δD) for spatial scales that span over 60° of latitude and temporal scales that cover the last century of global temperature increase.     

Distribution of boron in the environment

The findings of a study to identify and quantify the orders of magnitude for major reservoirs and flows of boron (B) in the environment are outlined. The orders of magnitude for B reservoirs and flows arising through natural processes, such as the hydrological cycle and volcanism, are compared with those arising from anthropogenic activities, such as coal combustion and the extraction and use of borates for commercial purposes. The major stores and reservoirs for B have been identified, in order of magnitude, as the continental and oceanic crusts (10¹⁸ kg B), the oceans (10¹⁵ kg B), groundwater (10¹¹ kg B), ice (10¹¹ kg B), coal deposits (10¹⁰ kg B), commercial borate deposits (10¹⁰ kg B), biomass (10¹⁰ kg B), and surface waters (10⁸ kg B). The largest flows of B in the environment arise from the movement of B into the atmosphere from oceans, at between 1.3 * 10⁹ kg and 4.5 * 10⁹ kg B per annum. Other hydrological flows are also important. Drainage from soil systems into groundwaters and surface waters accounts for between 4.3 * 10⁸ kg and 1.3 * 10⁹ kg B per annum. B mining and volcanic eruptions represent the next most significant B flows, accounting for approx 4.0 * 10⁸ kg and 3.0 * 10⁸ kg B, respectively.     

三峡水库消落带植被高程梯度分异及其对生境胁迫的响应

三峡水库蓄水运行形成的极端生境胁迫深刻改变了消落带植被结构和功能。在消落带横向断面高程梯度上,植被生境具有典型的空间异质性。选取三峡水库典型自然恢复消落带,通过野外调查和室内分析,揭示了消落带自然演替植被的群落构成、物种多样性和生物量随高程梯度的分异特征,系统分析了极端淹水、侵蚀-沉积、土壤环境等生境胁迫类型对消落带植被高程梯度分异的影响。结果表明：①研究消落带适生植被以草本为主,共有15科25种23属,其中禾本科种类较多,但单属单种、单优群落现象明显;一年生和多年生草本分别占52%和48%,且一年生草本多在消落带上部定居,多年生草本主要在消落带下部聚集。②物种多样性指数与高程呈正相关趋势,在145-150m范围内较低,在160-170m范围内较高。③植被生物量为199.68-1211.2g/m²,总体呈现随高程增加而显著增加的趋势;受多种生境因子的复合胁迫影响,生物量随高程存在局部波动。④水库水位变动形成淹水时长、出露时令、淹水强度等是影响消落带植被生物量高程梯度分异的主导因子;侵蚀/沉积过程改变土层厚度、根层土壤持水能力和肥力条件,对植被生长产生重要影响;土壤水分和氮是植被生长的限制性因子。因此,优势生境适宜性物种选育、土壤基质保育和植被格局功能优化是三峡水库消落带植被恢复和生态功能重建的重要任务。     

Progress and opportunities in advancing near-term forecasting of freshwater quality

Near-term freshwater forecasts, defined as sub-daily to decadal future predictions of a freshwater variable with quantified uncertainty, are urgently needed to improve water quality management as freshwater ecosystems exhibit greater variability due to global change. Shifting baselines in freshwater ecosystems due to land use and climate change prevent managers from relying on historical averages for predicting future conditions, necessitating near-term forecasts to mitigate freshwater risks to human health and safety (e.g., flash floods, harmful algal blooms) and ecosystem services (e.g., water-related recreation and tourism). To assess the current state of freshwater forecasting and identify opportunities for future progress, we synthesized freshwater forecasting papers published in the past 5 years. We found that freshwater forecasting is currently dominated by near-term forecasts of water quantity and that near-term water quality forecasts are fewer in number and in the early stages of development (i.e., non-operational) despite their potential as important preemptive decision support tools. We contend that more freshwater quality forecasts are critically needed and that near-term water quality forecasting is poised to make substantial advances based on examples of recent progress in forecasting methodology, workflows, and end-user engagement. For example, current water quality forecasting systems can predict water temperature, dissolved oxygen, and algal bloom/toxin events 5 days ahead with reasonable accuracy. Continued progress in freshwater quality forecasting will be greatly accelerated by adapting tools and approaches from freshwater quantity forecasting (e.g., machine learning modeling methods). In addition, future development of effective operational freshwater quality forecasts will require substantive engagement of end users throughout the forecast process, funding, and training opportunities. Looking ahead, near-term forecasting provides a hopeful future for freshwater management in the face of increased variability and risk due to global change, and we encourage the freshwater scientific community to incorporate forecasting approaches in water quality research and management.     

Relationships between river flows and recreational catches of Australian bass

The relationship between river flows, summarized by hydrological indices, and catches of Australian bass Macquaria novemaculeata from recreational fishing competitions were examined in the Hawkesbury‐Nepean River system. Between 55 and 198 fishermen took part in six monthly fishing competitions. The number of hours fished increased from 570 to 1800 h between 1998 and 2001. A total of 11 275 Australian bass were caught over the study period. The percentage of young‐of‐the‐year (YOY) Australian bass and the catch of fish per unit effort was influenced by either the flow regime occurring in the same year and flow in the previous year. The number of Australian bass caught per unit effort was positively associated with the median volume of water and the number and duration of high flow events occurring in the previous year. The percentage of YOY Australian bass caught in any one year was positively associated with the median flow in the same year of capture and the maximum, mean and variation of daily flows, the number and duration of high flow events and the greatest rise and fall of daily flows in the previous year.     

Stream type diversity in the Atlantic lowland of the Jureia area (Subtropical Brazil)

Different combinations of the three basic streaming water types in the Jureia area (São Paulo), namely blackwater with low pH, clearwater with low pH and estuarine water, are described. The hydrological situation is compared to that of the Amazonian basin and some paleolimnological and potamological observations are added.Scientific Contribution No. 6 from the Jureia Ecological Station (São Paulo, Brasil).Scientific Contribution No. 6 from the Jureia Ecological Station (São Paulo, Brasil).