Abundance of terrestrial gymnamoebae at a northeastern U. S. site: a four-year study, including the El Niño winter of 1997-1998

ABSTRACT. The abundance, sizes, and when appropriate, diversity of gymnamoebae were documented at approximately monthly intervals for four years (1995–1998) at a grassy, terrestrial site slightly upslope from a freshwater pond. Soil samples were analyzed for viable gymnamoebae using a standard laboratory culturing protocol. The mean density of gymnamoebae based on the total data set was ca. 1,600/g (s.e. ± 190). Minimum densities of gymnamoebae (156/g) occurred in January 1995, and a maximum for the sampling period (5,838/g) occurred in July 1997, when a rainy period followed an extended period of drought. Among the environmental variables monitored (precipitation, soil moisture, organic content, and temperature) only precipitation correlated significantly with abundance of gymnamoebae (r= 0.34 , p = 0.02 ). During the mild, moist El Niño winter of 1997–1998, a larger than usual number of gymnamoebae was recorded at the site (～3,800/g) compared to a mean density of ～900/g for comparable periods in preceding years. The mean sizes were also larger. Since gymnamoebae are increasingly recognized as major members of soil microbial communities enhancing soil fertility through nutrient mineralization, it is important to document environmental variables that influence their abundance and activity in terrestrial ecosystems.     

The density and diversity of gymnamoebae associated with terrestrial moss communities (Bryophyta: Bryopsida) in a northeastern U.S. forest

Moss communities are commonly found in temperate forests and form a nearly continuous understory in some high latitude forests. However, little is known about the microbial component of these communities, especially the non-testate amoeboid protists. Fifty morphospecies of naked amoebae were identified in samples collected at eight sites in a northeastern North American forest. The mean number (+/-SE) of morphospecies found per sample site based on laboratory cultures was 17+/-2.1. The density of amoebae expressed as number/g dry weight of moss ranged from 3.5+/-0.04 x 10(3) to 4.3+/-0.2 x 10(4) and was positively correlated with the moss moisture content (r=0.9, P<0.001, df=26). Densities of gymnamoebae in the moss are generally higher than found in the surrounding soil, but this may be due in part to the greater weight of soil per unit volume compared with moss. The percentage of encysted forms was inversely related to the moisture content of the moss sample.     

A comparison of vascular vegetation and protozoan communities in some freshwater wetlands of Northern Lower Michigan

Vascular vegetation and protozoan communities were sampled in seven wetland sites — two bogs, two fens, two marshes, and one swamp — in summer 1977. Two similarity indices were used to compare vascular vegetation and Protozoa from each site with all the other sites. Bog sites were the most distinct from other wetland types with respect to chemical and physical characteristics, dominant vascular vegetation, and protozoan species composition. The swamp site had the highest similarity to all other sites with respect to both dominant vascular vegetation and protozoan species. Protozoan communities from different wetland types were much more similar than dominant vascular species; however, the pattern of similarity between wetland sites was very similar for both groups (Pearson product-moment correlation coefficient = 0.76).Protozoan communities were also compared with those from several nearby lakes with respect to colonization rate onto polyurethane foam artificial substrates. The structure and dynamics of protozoan communities of wetlands were broadly different from those of other freshwaters, and somewhat unique to the other wetland types. Evidence for a high degree of eutrophy in certain bog lakes is presented.     

长白山不同海拔梯度裸肉足虫群落分布特征

裸肉足虫作为联结微生物和大中型土壤动物的重要环节, 在土壤生态系统物质循环和能量流动过程中起着重要作用。为探明裸肉足虫群落沿海拔梯度的分布特征及其主要驱动因子, 作者在长白山北坡选择不同海拔梯度(700 m、1,000 m、1,300 m、1,600 m、1,900 m和2,200 m), 采用最大可能数法对裸肉足虫进行了培养计数, 并采用平板培养、标记、分离再培养的方法进行了分类鉴定, 分析比较了不同海拔梯度裸肉足虫的群落组成和结构特征。结果表明: 长白山北坡裸肉足虫物种丰富, 不同海拔梯度裸肉足虫丰富度指数存在显著差异, 且与土壤酸碱度呈极显著正相关关系。其中林分较为单一的岳桦(Betula ermanii)林带(1,900 m)裸肉足虫丰富度最低, 位于植被交错带的针阔混交林带(1,000 m)裸肉足虫丰富度最大, Shannon-Wiener多样性指数和Pielou均匀度指数在不同海拔梯度间不存在显著性差异, 但变化趋势与丰富度一致。聚类分析结果显示, 1,300 m、1,600 m和1,900 m海拔带以及700 m和2,200 m海拔带裸肉足虫群落组成较为相似。典范对应分析(canonical correspondence analysis, CCA)显示, 裸肉足虫群落组成和结构主要受土壤酸碱度、铵态氮以及碳氮比的影响, 而海拔和土壤含水量对其没有显著影响。综上, 裸肉足虫群落多样性随海拔梯度的增加并未呈现递减或单峰的变化趋势, 土壤的基本理化性质是驱动裸肉足虫群落分布的主要因素; 此外, 地上植被也可能通过凋落物和根系分泌物间接影响裸肉足虫的群落组成和多样性。     

Densities and Diversity of Gymnamoebae in Relation to Some Inshore Aquatic Habitats at Bermuda

ABSTRACT Densities and diversity of gymnamoebae are reported for three sites at Bermuda. Two are marine sites in Mullet Bay, and the third is a shallow pond (Ferry Reach Park), Bermuda. Site 1 (edge of a small island in Mullet Bay) had higher densities of gymnamoebae (28,761/g sediment) than at a disturbed site 2 (17,597/g), a boat mooring. The diversity was higher, however, at site 2 (H = 4.3) compared to site 1 (H = 3.3). The site 2 species were larger including morphotypes categorized as type 1 (e.g. Mayorella and a reticulate amoeba). The brackish inland pond had higher abundances in the sediments (40.590/g) compared to the marine habitats. However, the diversity was lower (H = 2.7) and it was dominated largely by Vannella and Platyamoeba (categorized as morphotype 4). These data are consistent with findings at continental coastal locations in northeastern USA. Pond sediments generally contain higher densities of gymnamoebae than marine coastal sediments with less organic content. The ratio of type 4 to type 1 amoebae in pond samples is higher than those from coastal sites. The data from Bermuda, an open ocean insular site, provide additional zoogeographic evidence for the generality of these patterns of abundance.     

Three New Limax Amoebae Isolated from Marine Surface Sediments: Vahlkampfia caledonica N. Sp., Saccamoeba marina N. Sp., and Hartmannella vacuolata N. Sp.

ABSTRACT. Three new limax amoebae, isolated from marine, surface sediment samples are described using light microscopic and fine structural features. One species, characterized by eruptive locomotion typical of the family Vahlkampfiidae, is assigned the name Vahlkampfia caledonica (47.4 ± 16.0 μm × 12.1 ± 3.2 μm). The other two monopodial species move with steady locomotion characteristic of the family Hartmannellidae. One is a Saccamoeba with a distinct posterior bulbous uriod, vaculoes containing prominent crystals, glycocalyx with cup-like components, and spherical nucleus with central nucleolus. It is assigned the name Saccamoeba marina (72.5 ± 14.9 ±μm × 20. 7 ± 4. 5 μM). The other hartmannellid limax amoeba moves by steady locomotion and has a rather constant monopodial from, lacks a uroid, but has occasional trailing masses of cytoplasm, contains cup-like structures in the glycocalyx, and is characterized μm). Few limax amoebae have been described from marine environment and these data provide additional evidence that limax amoebae may be more abundant in marine sediments that realized previously.     

Trigonella arcuata-associated rhizobia��an Ensifer (Sinorhizobium) meliloti population adapted to a desert environment

Long-term monitoring of soil properties reveals site-specific ecosystem shifts in soil processes due to land use and climate changes. This paper aims to study the effects of physical landscape changes associated with grazing on soil thermal and moisture regime at the plot scale in a semiarid Leymus chinensis steppe of Inner Mongolia, China. The investigated sites were subjected to three grazing intensities: ungrazed since 1979 (UG79), moderately grazed only in winter time (WG), and heavily grazed (HG). At each plot, we recorded the soil moisture and temperature over a 6-year period that spanned between June 2004 and September 2009 and experienced a large range in precipitation (162 to 362 mm). Based on these monitoring data, we divided a year into four hydric periods: (1) growing period (late April to August); (2) transitional period from summer to winter (September?COctober); (3) winter time (November?Cfirst March); and (4) transitional period from winter to summer (March?CApril). In general, soil moisture in grazed sites was lower than in the ungrazed site, particularly for the 30?C50 cm soil layer. Seasonal fluctuation of the soil moisture, due to variable precipitation and atmospheric demands, was most significant in the topsoil (0?C10 cm) and was less pronounced in deeper soil. Regardless of hydric seasons, soil moisture was significantly influenced by grazing intensity, whereas soil temperature was slightly influenced. With increasing grazing intensity, soil water storage decreased remarkably. Consequently, grazing reduced plant available water and therefore grassland productivity, which are linked to a great extent with the trampling-induced soil structure change and soil moisture regime.     

Seasonal variations in the spatial distribution of root tips in teak (Tectonia grandis Linn. f.) plantations in the Varanasi Forest Division,India

Summary Seasonal variations in the spatial distribution of root tips were studied in 19 and 29 year old teak plantations, located on red and alluvial soils respectively. The pattern was essentially similar at both sites, but generally the alluvial soil site exhibited a greater number of root tips. Root tips decreased with increasing distance from the tree base. Through-out most of the year the relative distribution of root tips decreased with depth; the difference between 0–10 and 10–20 cm depths was marginal, but 20–40 cm depth contained distinctly fewer root tips. At all distances a similar seasonal trend was noticed, a mid rainy season peak being followed by a steady decline until the dry summer except for an abrupt rise to a smaller peak in February after the winter rains.The root tip density was positively correlated with the 2 mm root biomass and both showed a similar bimodal annual cycle. Of three environmental variables studied, soil moisture and rainfall were significantly positively correlated with root tip densityl the relationship between soil temperature and root tip density was negative and non-significant. The combined effect of soil moisture and temperature on root tip density, evaluated by a multiple regression model, accounted for 80–95% of the variation in root tip density.     

Infectivity variation of Discaria trinervis-nodulating Frankia in Patagonian soil according to season and storage conditions

Changes in the infectious capacity of soilborne Frankia from the same site may depend on environmental conditions. To test this, we examined the effect of season of sampling, sample storage protocol and storage time. The nodulation capacity of Frankia from rhizospheric soils of Discaria trinervis (Hook et Arn.) Reiche (Rhamnaceae) growing in northwest Patagonia (Argentina) was measured using the most probable number method. Soil samples were collected seasonally and either stored moist at 4°C or air dried at room temperature for few days. Old (air-dried) soil samples were also assayed. All soils nodulated D. trinervis seedlings. Nodulation units (NU) ranged from 44 (spring, moist storage) to about 1 ml⁻¹ of soil (summer moist, and summer and autumn, air-dried storage), with intermediate values in other samples. Soils stored for 12 years, 6 months or 1 week had similar NU. Frankia NU positively correlated with soil water content ( r = 0.6, P < 0.05); therefore, it is likely that soil moisture is a relevant factor regulating soilborne Frankia nodulation ability in Patagonian soils. We suggest that Frankia can remain as spores or grow saprophytically in Patagonian soils.     

Water-use efficiency of one C3 and two C4 grasses in response to varying soil moisture and herbage-removal levels in a seasonally dry tropical region

In a seasonally dry tropical region the water use efficiency (WUE) of three grasses (C₃ winter annualPolypogon monspeliensis, C₄ perennialDichanthium annulatum and C₄ warm seasonal annualEchinochloa colonum) was evaluated during summer and winter under nine experimental conditions (3 soil moisture×3 herbage removal). Generally leaf water status and transpiration rate decreased with soil moisture stress and increased with clipping intensity. During winter the transpiration rate of Dichanthium was much lower than that of Polypogon and its own rate in summer. Both soil moisture stress and clipping intensity increased the WUE in all instances. Despite differences in photosynthetic type, growing season and life form, these grasses exhibited broadly similar positive relationships, across nine treatments for WUE: soil moisture stress, and water consumption: production. The range of WUE (g. mm^–1) calculated on TNP through the nine treatments was: summer—Dichanthium 2.9–10.0, Echinochloa 2.0–6.7; winter—Dichanthium 4.3–36.3, Polypogon 1.9–12.0.     

Pan-Arctic soil moisture control on tundra carbon sequestration and plant productivity

Long-term atmospheric CO₂ concentration records have suggested a reduction in the positive effect of warming on high-latitude carbon uptake since the 1990s. A variety of mechanisms have been proposed to explain the reduced net carbon sink of northern ecosystems with increased air temperature, including water stress on vegetation and increased respiration over recent decades. However, the lack of consistent long-term carbon flux and in situ soil moisture data has severely limited our ability to identify the mechanisms responsible for the recent reduced carbon sink strength. In this study, we used a record of nearly 100 site-years of eddy covariance data from 11 continuous permafrost tundra sites distributed across the circumpolar Arctic to test the temperature (expressed as growing degree days, GDD) responses of gross primary production (GPP), net ecosystem exchange (NEE), and ecosystem respiration (ER) at different periods of the summer (early, peak, and late summer) including dominant tundra vegetation classes (graminoids and mosses, and shrubs). We further tested GPP, NEE, and ER relationships with soil moisture and vapor pressure deficit to identify potential moisture limitations on plant productivity and net carbon exchange. Our results show a decrease in GPP with rising GDD during the peak summer (July) for both vegetation classes, and a significant relationship between the peak summer GPP and soil moisture after statistically controlling for GDD in a partial correlation analysis. These results suggest that tundra ecosystems might not benefit from increased temperature as much as suggested by several terrestrial biosphere models, if decreased soil moisture limits the peak summer plant productivity, reducing the ability of these ecosystems to sequester carbon during the summer.     

Soil and xylem water potential and soil water content in contrasting Pinus contorta ecosystems,Southeastern Wyoming,USA

Summary The relationships between volumetric soil water content (), in situ soil water potential (_soil) and predawn xylem pressure potential (_predawn) were quantified in four contrasting lodgepole pine ecosystems in Wyoming, USA. On three of the sites, changes in _soil correlated closely with _predawn, but on a porous soil derived from coarse granitic parent material, _predawn declines occurred much sooner than corresponding declines in _soil, possibly because of local depletion of rhizosphere moisture and low molecular diffusivity of water in that soil. Exptrapolation of laboratory-derived characteristic curves for soil moisture to field conditions yielded different relationships between and _soil than curves derived from in situ measurements, probably because of disruption of soil structure and porosity during sample collection and handling in laboratory studies. Although a close correlation between and _predawn was observed, future efforts at modelling the soil-plant-atmosphere continuum should be directed towards a more detailed understanding of the complex relationships between _soil at varying depths and plant water stress.     

Density and diversity of protozoa in some arid Australian soils

This is the first extensive study of soil protozoa of arid lands. Twenty-six samples from litters, soils, termitaria, and a cyanobacterial crust, collected from central and south Australian arid lands, were analyzed for numbers and species of gymnamoebae, ciliates, and testacea. Amoebae ranged from 1,000-5,000/g of material, and were two orders of magnitude more abundant than ciliates. Both groups increased in abundance and species richness from bare soils through spinifex to mulga to chenopod vegetations. Testacea ranged 900-5,000/g with similar species richness throughout vegetations, but reached 11,900/g with a doubling of species in a refugium in Kings Canyon. The most prevalent species of amoebae, ciliates, and testacea were taxa associated with ephemeral and disturbed habitats (r-selection). The cyanobacterial crust might be considered a micro-refugium because it contained a number of non-encysting protozoa, including Thecamoeba sp. and Nassula picta, feeding on cyanobacterial filaments. The numbers and species richness of protozoa under shrubs were greater than in bare soils, supporting the resource island hypothesis that desert plants create soil heterogeneity by localizing soil fertility under their canopies.     

Evidence for three “classes” of microtubules in the interpolar space of the mitotic micronucleus of a ciliate and the participation of the nuclear envelope in conferring stability to microtubules

Exposure of Nyctotherus ovalis to low temperatures or vinblastine caused similar reactions of classes of microtubules (mt) present in the mitotic micronucleus of this ciliate towards both treatments. However, differences of sensitivity between certain classes of mt at individual mitotic stages exist. Unlike the kinetochore mt (kmt) of most other eukaryotic cells, kmt in Nyctotherus completely disassemble after incubation at 6–8 ° C (60 min) and most disappear after prolonged exposure to vinblastine (10^–5 M, 16 h). The depolymerization of kmt causes the collapse of the spindle and a dislocation of chromosomes at metaphase, yet the reduced number of kmt after vinblastine-treatment still allows an alignment of composite complexes at the spindle equator. The data suggest that three individual sets of mt exist in the interpolar spindle region during ana- and telophase: 1) interpolar mt (int mt), which are assembled during anaphase, are cold- and vinblastine sensitive; 2) manchette mt (ma mt), which are first observed underneath the nuclear envelope during mid-anaphase, are cold-stable and insensitive to vinblastine treatment (10^–5 M); after prolonged treatment (16 h) they form spiral structures; 3) stembody mt (st mt), comprising the interpolar region of the nucleus during telophase, are cold- and vinblastine insensitive. Paracrystalline structures resembling a stembody are formed in telophase-like division stages after prolonged vinblastine exposure (16 h, 10^–5 M). Since kmt and int mt possess the same sensitivity under depolymerizing conditions, they probably have a similar composition. Thus the idea that the int mt in this organism arise by elongation of kmt is supported. However, st mt apparently do not originate from an extension of preexistent int mt, but appear to represent a new set of stable mt. This is emphasized not only by their greater stability compared to the int mt but also by the distribution of cold-stable mt in late anaphase micronuclei. The ma mt may be an intermediary step in formation of st mt since their stability resembles that of the st mt. A comparison of the substructure of vinblastine-induced paracrystals in Nyctotherus with those observed in in vitro systems with known composition suggests that a turnover of MAPs may be responsible for the different stability of mt and thus could specify and regulate mt sensitivity and function. Another organelle, possibly involved in conferring stability to mt, is the nuclear membrane. The assumption that the nuclear envelope possesses an intrinsic property to nucleate mt and thus aid in the alignment of mt is supported.     

黄土高原水蚀风蚀交错区植被地上生物量及其影响因素

采用野外调查的方法,于2009年9月下旬测定了六道沟小流域不同土地利用方式下的地上生物量以及土壤水分含量和养分含量,研究了水蚀风蚀交错区典型小流域植被地上生物量水平及其影响因素.结果表明:六道沟小流域主要植被地上干生物量在177～2207g·m-2;其中,玉米、谷子、弃耕地、人工草地、天然草地和灌木地的地上干生物量分别为2097～2207、518～775、248～578、280～545、177～396和372～680 g·m-2.农田平均土壤含水量(0～100 cm土层)最高,达14.2%,灌木地最低,为10.9%;弃耕地土壤水分含量的变异系数最大,为26.7%,说明弃耕地土壤水分有很强的空间异质性.土壤平均储水量大小顺序为:农田>人工草地>弃耕地>天然草地>灌木地,苜蓿地和柠条地出现土壤干化现象.植被地上干生物量与0～100 cm土层土壤储水量存在显著正相关关系(r=0.639,P<0.05),地上鲜生物量与植被的株高呈极显著正相关,较高植被的地上生物量可以间接控制水蚀风蚀交错区土壤侵蚀.植被地上生物量与土壤水分、养分具有很高的相关性,但与海拔、坡度、坡向、容重等的相关性不显著.     

Patterns and drivers of Araucaria araucana forest growth along a biophysical gradient in the northern Patagonian Andes: Linking tree rings with satellite observations of soil moisture

Araucaria araucana (Araucaria) is a long‐lived conifer growing along a sharp west–east biophysical gradient in the Patagonian Andes. The patterns and climate drivers of Araucaria growth have typically been documented on the driest part of the gradient relying on correlations with meteorological records, but the lack of in situ soil moisture observations has precluded an assessment of the growth responses to soil moisture variability. Here, we use a network of 21 tree‐ring width chronologies to investigate the spatiotemporal patterns of tree growth through the entire gradient and evaluate their linkages with regional climate and satellite‐observed surface soil moisture variability. We found that temporal variations in tree growth are remarkably similar throughout the gradient and largely driven by soil moisture variability. The regional spatiotemporal pattern of tree growth was positively correlated with precipitation (r = 0.35 for January 1920–1974; P < 0.01) and predominantly negatively correlated with temperature (r = ?0.38 for January–March 1920–1974; P < 0.01) during the previous growing season. These correlations suggest a temporally lagged growth response to summer moisture that could be associated with known physiological carry‐over processes in conifers and to a response to moisture variability at deeper layers of the rooting zone. Notably, satellite observations revealed a previously unobserved response of Araucaria growth to summer surface soil moisture during the current rather than the previous growing season (r = 0.65 for 1979–2000; P < 0.05). This new response has a large spatial footprint across the mid‐latitudes of the South American continent (35°–45°S) and highlights the potential of Araucaria tree rings for palaeoclimatic applications. The strong moisture constraint on tree growth revealed by satellite observations suggests that projected summer drying during the coming decades may result in regional growth declines in Araucaria forests and other water‐limited ecosystems in the Patagonian Andes.     

Ecological optima and tolerances of Thelypteris limbosperma,Athyrium distentifolium,and Matteuccia struthiopteris along environmental gradients in Western Norway

The distribution and abundance of Thelypteris limbosperma, Athyrium distentifolium, and Matteuccia struthiopteris are modelled statistically in relation to 14 environmental variables along the major climatic, topographic, and edaphic gradients in western Norway. The data are from 624 stands from which measurements or estimates of mean January and mean July temperatures, humidity, altitude, aspect, and slope are available. From 182 of these stands eight soil variables have also been measured. The species responses are quantified by two numerical methods: Gaussian logit regression and weighted averaging (WA) regression. The estimated WA optima suggest that A. distentifolium has an ecological preference for low July and January temperatures, high altitudes, and soils of low-medium pH and base content. The species shows statistically significant Gaussian responses with summer temperature, humidity (= Martonnes humidity index), altitude, slope, aspect, pH, cation exchange capacity, and base saturation with optima of 8.7 °C, 188.9, 1220 m, 28°, 29°, 4.8, 13.77 mEq 100 g dry soil^-1, and 13.4%, respectively. These suggest that the occurrence and relative abundance of A. distentifolium are well predicted by summer temperature, topography, and soil pH and base status. T. limbosperma has WA optima that suggest that it favours moderately high winter and summer temperatures, high humidity, medium altitude, and soils of low pH and base content. It has significant Gaussian responses to summer temperature (optimum =12.6 °C), winter temperature (-1.8 °C), humidity (179.2), altitude (459.5 m), slope (22.5°), and Na (0.7 mg 100 g dry soil^-1). These suggest that climatic factors, altitude, and slope are significant predictors for its occurrence and abundance. M. struthiopteris has high WA optima for summer temperature, pH, Ca, Mg, K, Na, cation exchange capacity (CEC), and base saturation, and a low optima for humidity and winter temperature. Of these, summer temperature (16.0 °C), Ca (63.1 mg 100 g dry soil^-1), Mg (41.0 mg 100 g dry soil^-1), K (23.6 mg 100 g dry soil^-1), Na (5.0 mg 100 g dry soil^-1), CEC (60.7 mEq 100 g dry soil^-1), and base saturation (56.3%) have significant Gaussian logit responses, as do aspect (150.2°) and loss-on-ignition (9.4%). These results suggest that the occurrence and relative abundance of M. struthiopteris are well predicted by high soil base cations, a generally southern aspect, low organic content in the soil, and high July temperatures.     

Effects of aqueous extracts from leaves and leaf litter on the abundance and diversity of soil gymnamoebae in laboratory microcosm cultures

The distribution and abundance of microbiota in soil and litter may be significantly affected by the quality and quantity of localized patches of leaf organic matter. This study examined the relative effects of aqueous extracts of shed autumn leaves from American beech (Fagus grandifolia), sugar maple (Acer saccharum), red oak (Quercus rubra), and white oak (Quercus alba) on the density and diversity of gymnamoebae in laboratory cultures. Overall, the beech leaf extract produced the most growth of gymnamoebae followed by white oak with leaf extracts from maple and red oak producing least growth. Cultures using natural leaf litter from beneath beech trees had higher densities and diversity of gymnamoebae than leaf-litter cultures from a maple-oak stand. Soil microcosms confirmed that beech leaf extracts produced a higher density of gymnamoeba growth when added to soil cultures compared with maple and oak leaf extracts. Protein content, CHN (carbon and nitrogen content), and pH of the leaf extracts were assayed, but these alone were not sufficiently different to account for the effects. A dilution experiment indicated that some other concentration-dependent factor in the extract may produce the effects.     

Annual soil respiration in broadleaf forests of northern Wisconsin: influence of moisture and site biological,chemical, and physical characteristics

Soil temperature and moisture influence soil respiration at a range of temporal and spatial scales. Although soil temperature and moisture may be seasonally correlated, intra and inter-annual variations in soil moisture do occur. There are few direct observations of the influence of local variation in species composition or other stand/site characteristics on seasonal and annual variations in soil moisture, and on cumulative annual soil carbon release. Soil climate and soil respiration from twelve sites in five different forest types were monitored over a 2-year period (1998–1999). Also measured were stand age, species composition, basal area, litter inputs, total above-ground wood production, leaf area index, forest floor mass, coarse and fine root mass, forest floor carbon and nitrogen concentration, root carbon and nitrogen concentration, soil carbon and nitrogen concentration, coarse fraction mass and volume, and soil texture. General soil respiration models were developed using soil temperature, daily soil moisture, and various site/soil characteristics. Of the site/soil characteristics, above-ground production, soil texture, roots + forest floor mass, roots + forest floor carbon:nitrogen, and soil carbon:nitrogen were significant predictors of soil respiration when used alone in respiration models; all of these site variables were weakly to moderately correlated with mean site soil moisture. Daily soil climate data were used to estimate the annual release of carbon (C) from soil respiration for the period 1998–1999. Mean annual soil temperature did not differ between the 2 years but mean annual soil moisture was approximately 9% lower in 1998 due to a summer drought. Soil C respired during 1998 ranged from 8.57 to 11.43 Mg C ha⁻¹ yr⁻¹ while the same sites released 10.13 and 13.57 Mg C ha⁻¹ yr⁻¹ in 1999; inter-annual differences of 15.41 and 15.73%, respectively. Among the 12 sites studied, we calculated that the depression of soil respiration linked to the drought caused annual differences of soil respiration from 11.00 to 15.78%. Annual estimates of respired soil C decreased with increasing site mean soil moisture. Similarly, the difference of respired carbon between the drought and the non-drought years generally decreased with increasing site mean soil moisture.     

Seasonal changes in inorganic and organic phosphorus in the soil of a riparian forest

This study addresses the temporal distribution of forms of phosphorus in the soil of a temporarily flooded riparian forest of the valley of the river Garonne (Southwest of France). A sequential extraction for forms of phosphorus of increasing chemical stability was used. During the study period (13 months), the forest was flooded a few days during March and May. In winter, resin-Pi concentration was high (26 g g^–1) in comparison to spring values (<9 g g^–1). NaHCO₃-Po, NaHCO₃-Pi or NaOH-Pi concentrations increased during winter (up to 74, 124 and 78 g g^–1 respectively) and decreased significantly during spring (32, 44 and 32 g g^–1 respectively). This pattern was attributed to simultaneous mineralization and plant uptake during the growing season and to the flood events (erosional processes and P-release). During summer and fall, resin-Pi concentration increased significantly (up to 26 g g^–1 in October). NaHCO₃-Po concentrations remained low during spring and summer (<33 g g^–1), and increased significantly in fall (>45 g g^–1 NaHCO₃-Pi or NaOH-Pi increased in late spring or summer (90 g g^–1 and 68 g g^–1 respectively). Increasing concentrations of the labile forms during late spring or summer were ascribed to the warm temperature and soil dryness that limited plant growth. HCl-Pi increased regularly after the floods (174 g g^–1 before the flood events to 254 g g^–1 after the floods). Residual P presented a similar pattern i.e. 214 g g^–1 and 279 g g^–1 respectively before and after the flood events. This pattern was attributed to a progressive incorporation of flood deposits to the soil.