Forage nutrient composition in the wet season in Benue state,Nigeria. I. Macrominerals and in vitro organic matter digestibility

Abstract

Seventy‐one forage samples were analyzed for their macromineral composition and forage in vitro organic matter digestibility (IVOMD) in three agricultural zones of Benue State, Nigeria. The zones consisted of Northern, Eastern, and Central zones, each of which were made up of four Local Government Areas. In each Local Government Area, grazing animals were monitored and forages corresponding to those consumed were collected during the peak of the wet season (June) and analyzed for their macromineral composition and IVOMD. Fewer number of forage samples were harvested from Northern and Eastern zones due to greater agricultural activities and infra‐structural land use which limited land space for grazing animals. Forage IVOMD ranged from 32% to 78.3% across all classes of forage and from 43.5% to 62.8% in the Local Government Areas. About 18% of total samples, exclusively from the Northern zone, showed forage IVOMD concentrations below 20%, probably resulting from grazing pressures and agricultural activities in the zone. Forages from the Northern zone were deficient in phosphorus (P), potassium (K), and sodium (Na) based on their criteria of adequacy. No deficiency levels were indicated in forage calcium (Ca) or magnesium (Mg). Northern and Eastern zones were in greatest need of mineral supplementation programs.     

Mineral concentrations of forages grazed by small ruminants in the wet season in benue state,Nigeria. II. Trace minerals and forage crude protein

Abstract

A total of 71 forage samples were analyzed for trace mineral and crude protein concentrations in three Agricultural zones of Benue State, Nigeria. The zones consisted of the Northern, Eastern, and Central zones, each of which was made up of four Local Government Areas. In each Local Government Area, grazing animals were followed and forages corresponding to those consumed were collected during the peak of the wet season (June) and analyzed for the nutrient composition. Deficiencies were observed in copper (Cu) and cobalt (Co) concentrations in all classes of forage, and in forage Cu and zinc (Zn) in all Local Government Areas in the Northern zone. A higher (P<0.05) forage Cu concentration was observed in legumes compared to other classes of forage in the Eastern zone. Concentrations of iron (Fe) and manganese (Mn) were considered adequate and their contents were not affected (P>0.05) by class of forage or Local Government Areas. In the Eastern zone, the contents of selenium (Se) in grass and tree leaf hay were higher compared to leguminous forage, which in turn was higher compared to Se concentrations in crop wastes. Only about 18% of total forage samples showed protein concentrations below the critical value of 7%. Supplementation of Cu, Zn, and Co would seem to be necessary in the Northern zone, and to a lesser extent in the Eastern zone for optimum productivity of grazing animals.     

Contribution of Farm-Radio Broadcasts to Yam Output in Benue State,Nigeria

This study analyzed farmers’ perceptions of the contribution of farm-radio broadcasts to yam production. Data collected from 200 randomly selected farmers in Benue State, Nigeria using a structured questionnaire showed that 94.0% considered hours of broadcasts (8 a.m., 11 a.m., 2:30 p.m., and 7 p.m.) suitable, 98.5% were satisfied with the language of broadcasts, 97.5% found the contents adequate, and 88.5% utilized the messages. The paired sample t test showed significant differences between yield of yams before and after listening to radio (p < .01), indicating farm-radio broadcasts’ contribution to productivity. It is recommended that farm-radio broadcasts be intensified and sustained to enhance output and food security.     

Frequency of defoliation and nitrogen and phosphorus fertilization on Andropogon gayanus Kunth. I. Yield,crude protein content,and in vitro digestibility

Abstract

An experiment was conducted in a semi‐arid region located in the State of Zulia, western part of Venezuela (10°32'N and 71°42'W, 600 mm average annual rainfall), to evaluate dry matter (DM) yield and in vitro organic matter digestibility (IVOMD), and crude protein (CP) content of Andropogon gayanus Kunth as affected by three frequencies of defoliation (every 42, 63, and 84 days) and fertilization with three levels of nitrogen (N) (0, 100, and 200 kg N ha^‐1‐year^‐1) and two levels of phosphorus (P) (0 and 75 kg P₂O₅ ha^‐1.year^‐1) in a factorial array using a split‐split‐plot experimental design with frequencies in the main plots, N in the sub‐plots, and P in the sub‐subplots with three replications. Soil was a sandy loam Aridisol with a pH of 5.5. Average soil calcium (Ca), magnesium (Mg), sodium (Na), potassium (K), and P contents were 0.6, 0.3, 0.1 and 0.17 meq‐100g^‐1 soil, and 6 ppm, respectively. Data from six, four, and three cuttings for the frequencies of 42, 63, and 84 days were analyzed over the total duration of the study (252 days) as well as separately for periods with high (168 days, 384 mm) and low rainfall (84 days, 69 mm). Frequency of defoliation was the only factor that influenced (P≤0.05) the variables studied. In the overall analyses, the highest (P≤0.05) DM yield (3,656 kg#lbha^‐1.cutting^‐1) was obtained with harvests every 63 days. Mean IVOMD decreased (P≤0.05) from 54.2 to 51.7% with increasing harvest interval from 63 to 84 days, respectively. The average CP content was 7.9%. With low rainfall, mean DM yield was 2,209 kg#lbha^‐1, CP content declined (P≤0.05) from 7.5 to 3.9% as the cutting interval increased, and IVOMD decreased (P≤0.05) between 42 and 63 days. With high rainfall, the highest (P≤0.05) DM yield (4,872 kg#lbha^‐1) and IVOMD (56.5%) were found at 63 days of age. Mean CP content was 9.3%. These results confirm that A. gayanus is a highly productive forage grass. Lack of response to N and P fertilizers may be attributed partly to relatively low rainfall during the experiment, adaptation of the grass to low fertility soils, and long intervals between N applications and the next harvest.     

In vitro digestibility and crude protein and mineral concentrations of guinea grass accessions in a humid tropical region of Puerto rico

Abstract

The in vitro organic matter digestibility (IVOMD), crude protein (CP) content and mineral composition of ten Panicum maximum accessions were compared between seasons in Puerto Rico and evaluated in relation to grazing ruminants requirements. On short days, PRPI 13605 was superior (P<0.05) in IVOMD to all the other accessions. In terms of the CP content, accession PRPI 3634 was above 11% in both seasons, however, without differing (P>0.05) from most accessions. The mean macroelement content of the accessions was generally adequate in relation to grazing ruminant requirements with the exception of Na and Mg. Phosphorus was less than the critical concentration (0.25%) for one‐half of the accessions in the short day season and 2 of 10 for the long day season. For all samples, Mn was high and Fe was generally adequate in relation to ruminant requirements. Most all samples contained deficient concentrations of Co, Cu, Se, and Zn. Forage Mo concentrations, therefore, did not result in conditioned Cu deficiencies. In this context, it is probable that Na, Se, Cu, Co, Zn, and perhaps Mg, will be needed even if intensive fertilization is practiced in the humid tropical region of Puerto Rico.     

Yield,in vitro digestibility,crude protein,and mineral concentration of eight Digitaria introductions in Puerto rico

Abstract

Dry matter (DM) yield, in vitro organic matter digestibility (IVOMD), crude protein (CP) and mineral composition of eight Digitaria accessions were compared between long‐ and short‐day seasons in the semiarid southern region of Puerto Rico and evaluated in relation to grazing ruminant requirements. Digitaria milanjiana 6416 was consistently among the highest DM yielding accessions in both seasons. The mean IVOMD was similar in both seasons for most accessions. Concentrations of CP, magnesium (Mg), copper (Cu), zinc (Zn), cobalt (Co), and selenium (Se) were below the recommended levels for grazing ruminants in both seasons. This study suggests the need for livestock mineral supplementation, even under conditions of high pasture fertilization (NPK) and forage‐growing conditions in the semiarid southern region of Puerto Rico.     

Mineral concentrations in leaves and stems of various forages of the Colombian paramo

Abstract

A study was conducted to determine the elemental composition of two plant fractions (leaves and stems) of several forage species in three sheep farms of the paramo in Colombia. The elemental composition of the forage species, and the relationship between soil chemistry and the elemental composition of the forages were also determined. Sampling periods corresponded to the end of the rainy season (May‐June 1987), and the middle end of the dry season (February 1988). Leaves were higher (P<0.05) than stems in the following: calcium, phosphorus, magnesium, potassium, iron, molybdenum, crude protein, and IVOMD. Overall percentage of deficiencies were related to the requirements for sheep as follows: calcium (88%, 13%), phosphorus (50%, 27%), magnesium (85%, 41%), potassium (13%,3%), sodium (94%, 96%), iron (10%, 4%), copper (82%, 65%), manganese (7%, 0%), zinc (46%, 42%), cobalt (92%, 85%), selenium (77%, 65%), crude protein (45%, 8%) for stems and leaves, respectively.

Based on analyses, elemental, crude protein and IVOMD concentrations of forage species, tended to differ. Soil‐forage correlation coefficients of the same mineral for the rainy season were calcium (r = 0.81), magnesium (r = 0.89), potassium (r = 0.71), zinc (r = 0. 69). For the dry season, correlations were calcium (r = 0.61) and magnesium ( r = 0.58). Results indicated low correlation coefficients between most soil and forage elements, and that they are not of great value in assessing the elemental status of grazing sheep in the paramo.     

Evaluating baseline data for trace elements,pH, organic matter content,and bulk density in agricultural soils in Nigeria

Agricultural soil samples were collected about 1 km apart over 21 km from 32 tilled/cultivated plots of yam, rice, and cassava in urban, rural, and the derelict Enyibga lead-zinc mine (EM) in the Abakaliki area, Nigeria during the rainy season in September, 1992. In the derelict mine, mean elemental contents increased in the order Cd < Ni < Cu < Mn < Pb < Zn; while in the urban, rural, and all soils combined, the order increased as follows: Cd < Cu < Ni < Pb < Zn < Mn. The overall mean distribution of all soils shows Mn and Zn to approach and exceed toxic levels, respectively. In all soils, the total mean concentrations of Cu and Ni are well below toxic levels. The Abakaliki area is less likely to be subjected to Cd-contaminated soils. Pb was excessively high at EM and, moderately high at Mgbowo Street in the urban area, but very less so in the rural areas. The rural agricultural areas of Agbaja, Nkwaegu, and Amaegu, including the isolated Ezza Road as well as the peripheral Expressway had relatively lower levels of heavy metals, pH and organic matter content than the urban conglomeration of Mile 50, Mgbowo Street, and Azuiyiokwu including the derelict mining village of Enyigba and EM; except that Ezza Road had pH and organic matter as high as the densely populated urban cultivated areas. The relationship between bulk density and organic matter was highly dependent on pH.     

Forms and profile distribution of potassium in typical soils of the lower Benue Valley of Nigeria

Abstract

Six profiles, derived from Precambrian Basement Complex rocks (mainly gneiss), Cretaceous sediments (mainly shale and sandstone), and Quaternary alluvium, and which are typical of the major agricultural soils in the Lower Benue Valley (Nigeria) were studied with the objective to determine their overall potassium (K) reserves and any relationship between these and other soil properties including their parent materials. Total K in the soils varies from 0.13–27.1 g kg^‐1 with average 6.64 g kg‐¹. This correlates positively with the clay, and negatively with the sand contents of the soils and is also influenced by their parent materials. The order of abundance according to parent material is: alluvium‐ > Basement Complex (gneiss)‐ ≈ shale‐ > sandstone‐derived soils. The concentrations of readily available K (RAK) in the soils are quite low, accounting for only between 0.30 and 7.8% of the total K in the soils and less than 4.0% of their exchange capacities. Based on critical limits established for many Nigerian soils, the soils derived from sandstone are clearly deficient in RAK, while soils developed from gneiss, shale and alluvium parent materials have moderate to sufficient levels for a wide range of crops. Non‐exchangeable or moderately available K (MAK) in the soils is also relatively low (0.020–8.59 mmol_c kg^‐1); while the sandstone‐derived soils have the least MAK, the alluvial soils have the most levels. However, the potassium supplying power (KSP) of the soils may be considered to be generally high. Although this bears no particular relationship to soil parent materials, the sandstone‐derived soils have the lowest KSP. The bulk of the total K reserves in the soils (55–88%) exists as difficultly available or structural K (DAK). The alluvial soils first, then the gneiss‐ and shale‐derived soils next have the highest contents of DAK, while the highly weathered sandstone soils have the lowest. Simple correlation analysis shows that, irrespective of parent material and K form, clay content and CEC are the most important soil properties influencing the overall K supplying status of these soils. It is concluded that in major agricultural soils of the Lower Benue Valley of Nigeria K exists mostly in the lattice structures of K‐bearing minerals, with accumulations in the subsurface horizons. Its plant‐available or supplying status is low on sandstone‐derived soils and moderate to sufficient on soils derived from Basement Complex rocks, shales and alluvium.     

Characterizing Farmer Users and Nonusers of Mass Media as Channels of Agricultural Information in Benue State,Nigeria

This study characterized farmer users and nonusers of mass media as channels of agricultural information. A structured interview was used to obtain data from 316 randomly selected farmers in Benue State, Nigeria. The data were subjected to discriminant analysis and the following socioeconomic characteristics significantly differed at a 5% level of probability between users and nonusers of mass media (and their F-ratio values): education (6.30), income (5.12), gender (4.84), and socioeconomic status (4.83). Farmer users of mass media are therefore those who have good level of education, belong to a relatively high income bracket, and are typically male and of a relatively high socioeconomic status. Farmers’ socioeconomic characteristics should be considered in planning mass media usage in agricultural information dissemination.     

Labile, recalcitrant, and inert organic matter in Mediterranean forest soils

The biochemical quality of soil organic matter (SOM) was studied in various profiles under Quercus rotundifolia Lam. stands on calcareous parent material. Special attention was paid to the question of how biochemical quality is affected by position within the soil profile (upper versus lower horizons). The following global SOM characteristics were investigated: (a) overall recalcitrance, using hydrolysis with either hydrochloric or sulphuric acid; (b) hydrolyzable carbohydrates and polyphenolics; (c) extractability by hot water and quality of the extract; and (d) abundance of inert forms of SOM: charcoal and soot-graphite. The recalcitrance of soil organic carbon (OC) decreases with depth, following the order: H horizons>A horizons>B horizons. In contrast, the recalcitrance of nitrogen is roughly maintained with depth. The ratio carbohydrate C to total OC increases from H to B horizons, due to the increasing importance of cellulosic polysaccharides in B horizons, whereas other carbohydrates are maintained throughout the soil profile at a relatively constant level, 12-15% of the total OC in the horizon. Whereas the quality of the hydrolyzable carbon (measured by the carbohydrate to polyphenolic C ratio) decreases with depth from H to B horizons, the quality of the hot-water extractable organic matter is much higher in B horizons than in A or H horizons. The relative importance of both charcoal and soot-graphitic C and N tends to increase with depth. The ratio black/total is usually higher for N than for C, a result that suggests that inert SOM may represent a relevant compartment in the nitrogen cycle. Overall, our data suggest that in Mediterranean forest soils the organic matter in B horizons could be less stable than often thought.     

In Vitro digestibility,crude protein,and mineral concentrations of Leucaena leucocephala accessions in a wet/dry tropical region of venezuela

Abstract

An experiment was conducted on a commercial farm located in the western part of Venezuela (10.5°N and 72°W; mean annual rainfall of 1000 mm; mean annual temperature of 28°C; sandy‐loam Alfisol with pH of 5.5). The purpose of the experiment was to evaluate the in vitro organic matter digestibility (IVOMD), crude protein (CP) content and mineral composition of four Leucaena leucocephala (Lam.) De Wit accessions under rotational grazing by heifers over a 6‐month period covering dry and rainy seasons, using a split‐plot experimental design with two replications. Neither accessions nor the accession x season interaction affected (P>0.05) any of the variables. The mean IVOMD was 68.6%, whereas CP content during the rainy season (26.5%) was higher (P<0.05) than in the dry season (24.3%). Average mineral content of the accessions were adequate in relation to grazing ruminant requirements with the exception of phosphorus [(P) 0.13%], sodium [(Na) 0.038%], copper [(Cu) 6.9 ppm], and zinc [(Zn) 19.7 ppm]. Forage P concentration may have been influenced by the low soil P content of the experimental site. The mean forage Ca:P ratio (11.3:1) was considerably wider than desirable. During the dry season, ash content increased (P<0.05), Na, iron (Fe), and cobalt (Co) decreased (P<0.05), but Fe and Co still remained above the critical levels. Mean concentrations of other elements were not affected (P>0.05) by season. Forage molybdenum (Mo) concentrations were low and, therefore, would not result in conditioned Cu deficiency. The four L. leucocephala accessions had similar feeding value for grazing ruminants and their quality was not markedly reduced in the dry season. Mineral supplementation of ruminants grazing this legume may be needed to correct specific deficiencies and imbalances.     

Mineral Concentrations of Cool Season Pasture Forages in North Florida During Winter-Spring Grazing Season. I. Macrominerals and Forage Organic Constituents

Two experimental late fall-winter-spring grazing studies, each lasting two years, were conducted at the North Florida Research and Education Center (NFREC), Marianna, Florida to evaluate the organic constituents and macromineral concentrations of annual cool season pasture forages grazed by growing beef cattle. Eight 1.32 ha fenced pastures or paddocks were divided into two pasture land preparation/planting methods, four pastures for the sod seeding treatments and four for the prepared seedbed treatments. These pastures were planted with two different forage combinations: rye/oats mix with or without ryegrass for the first two years (Study 1), and oats with ryegrass or ryegrass only for the last two years (Study 2). Each of the four forage/land preparation combination treatments was assigned to two pastures each year, thereby giving two replicates per year. Forage samples were collected at the start of grazing and twice monthly thereafter until the end of grazing season for each year, pooled by month, and were analyzed for calcium (Ca), phosphorus (P), sodium (Na), potassium (K), magnesium (Mg), dry matter (DM) yield, crude protein (CP), and in vitro organic matter digestibility (IVOMD). Blood plasma samples were also collected from the tester cattle during the spring season of year 2 of Study 2 and were analyzed for Ca, P, and Mg. Month differences were observed in forage concentrations of P and K (P < 0.0001), and Mg (P < 0.05) in both studies, Ca (P < 0.01) in Study 1 only, and Na (P < 0.05) only in Study 2. Year affected P, K, and Mg concentrations in Study 1 and Ca, P, and Na concentrations in Study 2. In Study 2, forage type by month interactions on Ca, K, and Mg concentrations were noticed (P < 0.01). Forage Ca was lower (P < 0.05) than the critical level for all months from the oat plus ryegrass pastures, and for early winter months and late spring months from ryegrass only pasture. Forage Na concentrations were consistently low throughout the grazing season and unaffected by forage type or land cultivation methods used in both studies. Low Mg concentrations of both forage types in Study 2 (also with high K concentrations) were indicative of a potential risk of grass tetany (hypomagnesemia) for grazing ruminants. Forage DM yields were highly variable with fluctuations among the experimental months and were found to be highest in the spring months, with decreasing yields towards the end of the grazing season in both studies (P < 0.0001). The CP concentrations were greater than the required levels and both CP and IVOMD decreased gradually by month in both studies (P < 0.0001). Normal blood plasma concentrations of Ca and P obtained were indicative of a good overall status of these minerals in the animal's body. Plasma Mg concentrations were slightly above the critical level for cattle from both forage types. In summary, the macrominerals most likely to be deficient in North Florida during the cool season would be Ca, Na, and Mg. Special attention should be given to supplementation of Mg since forages reflected a marginal deficiency of this mineral and high K concentrations were found.     

Calibration model of microbial biomass carbon and nitrogen concentrations in soils using ultraviolet absorbance and soil organic matter

There is a need for a rapid, simple and reliable method of determining soil microbial biomass (SMB) for all soils because traditional methods are laborious. Earlier studies have reported that SMB‐C and ‐N concentrations in grassland and arable soils can be estimated by measurement of UV absorbance in soil extracts. However, these previous studies focused on soils with small soil organic matter (SOM) contents, and there was no consideration of SOM content as a covariate to improve the estimation. In this study, using tropical and temperate forest soils with a wide range of total C (5–204 mg C g^?1 soil) and N (1–12 mg N g^?1 soil) contents and pH values (4.1–5.9), it was found that increase in UV absorbance of soil extracts at 280 nm (UV₂₈₀) after fumigation could account for 92–96% of the variance in estimates of the SMB‐C and ‐N concentrations measured by chloroform fumigation and extraction (P < 0.001). The data were combined with those of earlier workers to calibrate UV‐based regression models for all the soils, by taking into account their varying SOM content. The validation analysis of the calibration models indicated that the SMB‐C and ‐N concentrations in the 0–5 cm forest soils simulated by using the increase in UV₂₈₀ and SOM could account for 86–93% of the variance in concentrations determined by chloroform fumigation and extraction (P < 0.001). The slope values of linear regression equations between measured and simulated values were 0.94 ± 0.03 and 0.94 ± 0.04, respectively, for the SMB‐C and ‐N. However, simulation using the regression equations obtained by using only the data for forest profile soils gave less good agreement with measured values. Hence, the calibration models obtained by using the increase in UV₂₈₀ and SOM can give a rapid, simple and reliable method of determining SMB for all soils.     

In Vitro digestibility,crude protein content,and mineral concentrations of cynodon,brachiarin, and digitaria accessions in a humid tropical region of Puerto Rico

Abstract

The in vitro organic matter digestibility (IVOMD), crude protein (CP) content, and mineral composition of 11 grasses were compared between seasons in Puerto Rico and evaluated in relation to grazing ruminant requirements. Digitaria eriantha was the highest in IVOMD for both seasons, being higher (P<0.05) than 6 of 10 forages in the long‐day season and 4 of 10 in the shortday season. No differences (P>0.05) in CP content were observed among accessions at both seasons. Mean macroelement content of the accessions was generally adequate in relation to grazing ruminant requirements with the exception of sodium (Na) and magnesium (Mg). Forage microelement concentrations of cobalt (Co), copper (Cu), and zinc (Zn) were generally under the grazing ruminant requirements for the accessions evaluated during both seasons. Iron (Fe) and manganese (Mn) content were high in relation to requirements, especially during the short‐day season. Molybdenum (Mo) was not in excess for the accessions evaluated. The Zn concentrations were similar to the results reported from other experiments with higher fertilization levels. The selenium (Se) concentrations presented an apparent seasonal variation higher in the short‐day season, which is similar to other experiments with high fertilization levels.     

Mobilization and immobilization of dissolved organic matter in forest soils

Field and laboratory studies combined with destructive and nondestructive analytical methods were used to characterize dissolved organic matter (DOM) in acid forest soils. DOM is produced in significant amounts in the forest canopy and in the forest floor. A major part of the organic solutes are lignocellulose-degradation products being strongly microbially altered in the course of ligninolysis. The release of lignin-derived moieties into the soil solution is controlled by their degree of biooxidation. Microorganisms contribute also directly to the organic solutes through the release of microbial metabolites. DOM released from the forest floor passes the upper mineral soil almost conservatively, whereas in the subsoil most DOM is removed from solution. Immobilization of DOM is mainly due to sorption on Fe and Al oxides. The highly oxidized lignin-derived moieties are preferentially removed from the soil solution whereas the saccharides are relatively enriched. We conclude that DOM in the forest soil output to the hydrosphere is a result of (1) the release of microbially degraded lignocellulose compounds and of microbial metabolites into the forest floor solution and (2) selective sorptive removal of the lignin-derived constituents in the subsoil.     

山东省苹果园土壤有机质及养分状况研究

通过大量田间采样分析了山东省三种主要土壤类型苹果园土壤的有效养分状况及其分布特点 ,结果表明 :三种土壤类型果园土中有效养分含量差异较大 ,棕壤富磷贫钾 ,潮土富钾贫磷 ,褐土介于二者之间 .不同土层间有效养分含量有较大差异 ,表层土 (0～ 2 0cm)含量最高 ,底层土 (4 0～ 60cm)含量最低 ;丰产园三土层间有效养分含量差异较少 ,低产园差异较大 ;丰产果园三土层氮磷钾比例的平均值为 :0～2 0cm1∶0 .53∶1 .59;2 0～ 4 0cm为 1∶0 .53∶1 .69;4 0～ 60cm为 1∶0 .51∶1 .72 .与 1 0年前相比 ,果园土壤有机质含量降低 ,有效氮磷钾含量增加 ,其中磷钾增幅较大 .     

The nature and stability of organic phosphates in leaf litter and soil organic matter in Nigeria

The organic phosphorus components of leaf litter from a secondary forest in Nigeria were characterized as phospholipids, acid soluble esters, LiOH-extractable esters and residual phosphate. During incubation of the litter at 30°C for 8 months all four organic fractions were synthesized and the content of inorganic phosphate decreased.During cultivation of the same field site over a period of 22 months, the IP_{5 + 6}, content of the soil did not change significantly, but there were significant decreases of phospholipids and of high molecular weight components. The high molecular weight components, which were not identified, represented the most important source of organic phosphorus that became available to plants, but phospholipids may also have been a source.The results indicate that the inositol phosphates in leaf litter were in too low concentration to have provided the amounts found in the soil.     

Spatial microdistribution of mites and organic matter in soils and caves

Spatial variability is a key to understanding the structure and function of soil biodiversity. This research addressed the question of whether a mite centimetric spatial pattern corresponds to that of organic matter in two caves and in the mineral horizon of three forest soils. Therefore, different statistical tools were used and compared: classic aggregation analysis through variance-to-mean ratio and Morisitas index, nested hierarchical ANOVA and Morans I autocorrelation coefficient. The spatial pattern of organic matter was generally found to be of the gradient or patch type, influenced by slope and trees. Cave sediments far from the entrance contained smaller patches of organic matter than deep soil and cave entrances. Mite density spatial patterns sometimes corresponded to that of organic matter in soils but never in caves. Correlograms of mite species composition were significant in soils but not in caves. The difference between the space available in caves compared with that in the tortuous pores of soil is thought to be a major structuring factor for mites, by influencing their mobility. Correlograms were the most dependable spatial analysis tools, as they could be statistically tested and used to clarify the patterns detected by the nested hierarchical ANOVA method.