Cenozoic paleosols San Diego area,California

Ancient weathering profiles provide mute evidence of the major climatic regimes that operated in the southern California area during the Cenozoic Era. A tropical climate during part of the Paleocene and Early Eocene caused severe weathering of Jurassic andesitic rocks, Cretaceous granitic rocks and Late Cretaceous and Early Eocene terrigenous rocks. Erosional remnants of this paleosol exist as buried soils up to 30 meters thick and as exhumed soils on some modern hills. The main weathering horizon is overwhelmingly composed of kaolinite with residual quartz grains and minor amounts of iron oxides. This tropical climate was in effect at 35° to 40° north latitude.Late Eocene sedimentary rocks were deposited under a semi-arid climate with 50 to 60 cm of annual rainfall that was concentrated during one season. This interpretation is based on: 1) the dominance of conglomerate and immature sandstone in the Upper Eocene section compared to the relative scarcity of claystone, 2) the immaturity of the clay mineral suite which is dominated by smectite and vermiculite, 3) the presence of fractured clasts presumably split by growth and differential expansion of salts, 4) the multiple caliche beds that individually are up to one meter thick, and 5) the paleohydrology of the fluvial deposits which transported rhyolite gravels over 300 km distance from an eastern bedrock source about 4,000 m high in a river of 1.3 sinuosity with 100 year flood discharges up to 30,000 m³/sec.The extensive marine terraces in San Diego are mantled by relict soils that record composite weathering characteristics from glacial and interglacial climates from Late Pliocene to present. Maximal development of the paleosol includes an ironstone concretion layer (B_ir horizon) above an illuvial clay layer (B_t horizon) which rests on an iron- and silicacemented hardpan (C_m horizon).     

Modeling Herbicide Movement to Ground Water in Irrigated Sandy Soils of the San Joaquin Valley, California

A semi-empirical probabilistic transport model was developed to simulate simazine and diuron well water concentrations in an agriculturally intensive coarse soil region of Fresno County, California. Model inputs included five random variables: the organic carbon normalized soil adsorption coefficient, root zone degradation, application rate, depth to ground water, and ground water recharge age. Transport was simulated in two phases: initial transport through the root zone using the mechanistic model LEACHM, and a second empirically-based phase that simulated transport from the bottom of the root zone to the water table, and ultimately to domestic water wells. Best-fit calibration estimates for combined deep vadose/shallow ground water degradation half-lives were 330 d and 455 d for simazine and diuron, respectively. Simulations based on these fitted half-lives yielded coefficients of determination and root mean square errors of 0.973 and 0.993, and 0.367 and 0.364 for observed vs predicted simazine and diuron concentration percentiles, respectively. The calibrated model output also described the observed relationships of decreasing detection frequency and decreasing concentration with increasing depth to ground water. A novel contribution is the calculation of regional mass budgets for the herbicides. In modeling results, 9–54% and 2–16% (10th–90th percentiles) of applied simazine and diuron, respectively, leached out of the 1.5 m root zone, while the upper 10th percentile of well water concentrations corresponded to approximately 1–2% of application for both pesticides.     

Physical, chemical, and mineralogical characteristics of steppe paleosols of the ural region

Investigation of paleosols with different ages of burial mounds and the unique fortified city of Arkhaim in the steppe zone of the Southern Trans-Urals (Chelyabinsk region) is carried out. They are located on the remnants of the Big Karaganka River valley. The time of construction of archaeological monuments dates back to the Early Iron Age (Sarmatian Culture, 2300–2200 years ago) and Middle Bronze Age (Sintashta culture, 3800–4100 years ago). The soils are of medium and light loamy granulometric composition. Morphological, chemical, and mineralogical investigations of paleosols and background soils indicate that, in the Sarmatian time, the climatic conditions in the region were drier than currently, while during the Sintashta cultural development, the climate of the region was similar to the present one.     

Pampas deer conservation with respect to habitat loss and protected area considerations in San Luis, Argentina

Ozotoceros bezoarticus celer is the most endangered subspecies of pampas deer. Although common in the Argentine Pampas 100 years ago, it persists in only two small populations. The largest population has survived due to the rarity of roads, internal farm subdivisions, and the low cattle density. However, habitat condition for this population has changed dramatically in the last 16 years. Five Landsat images (1985, 1992, 1997, 1999, 2001), covering 4608 km², were used to quantify pampas deer habitat loss due to the replacement of natural grassland by exotic pastures and crops. Image classification showed that natural grassland cover was reduced from 84.5 to 37.8% between 1985 and 2001. The annual transformation rate increased significantly from 1.4 to 10.9%. Average paddock size was significantly reduced from 1470 to 873 ha, and the number of paddocks increased from 129 to 227. The land within this area proposed for a national park has not escaped these habitat changes. In the last 6 years the amount of replaced area within the proposed park has increased from 9.1 to 51.1% due to actions by ranchers to avoid inclusion within park boundaries. Three patches of natural grassland still remain within the pampas deer distribution, one of which is the proposed national park. The implementation of a national park is a decisive challenge for the survival of pampas deer and its habitat in Argentina.     

Late Quaternary paleosols and their paleoenvironmental significance along the Andean piedmont,Eastern Bolivia

The Andean piedmont of eastern Bolivia is situated at the southern margin of Amazonia characterized by an overall humid climate regime with a marked contrast between the rainy and dry seasons. The nearby Subandean foothills deliver abundant sandy sediments to the piedmont, leading to a complex array of sediments and paleosol horizons. Within this setting, the presented study analyzes four profiles of paleosol-sediment-sequences along incised ephemeral streams near Santa Cruz de la Sierra with a focus on past pedogenic variability in the context of the regional late Quaternary geomorphic and environmental evolution.     

Cenozoic sediments,soils and climates at whyalla,South Australia

A stratigraphic sequence of Cenozoic sediments and soils occurs in the Whyalla area (South Australia). During formation of the oldest soil layer, in pre-Cenozoic rocks, quartzites and sandstones were little altered but the less resistant rocks were strongly weathered to great depths. The resulting deep soil was destroyed in most places during an ensuing period of erosion, but competent water transportation removed most of the detritus. By the end of this erosional period the major features of the present topography had evolved.     

Late Quaternary alluvial fans and paleosols of the Kangra basin,NW Himalaya: Tectonic and paleoclimatic implications

The paper describes Late Quaternary pedosedimentary sequences of the alluvial fans from the Kangra basin of NW Himalayas for tectonic and paleoclimatic implications. In the proximal part of the Kangra basin three coalescing alluvial fans, namely Rait-Rihlu fans (~ 65 km²), Kangra fans (~ 200 km²), and Palampur fans (~ 170 km²) from west to east evolved due to reactivation of longitudinal and transverse faults and climatic changes during the Late Quaternary. The fans are characterised by subsidence of Rait-Rihlu fans, uplift of Kangra fans and tilting of Palampur fans. The thick (~ 90 m) pedosedimentary sequences exposed along the rivers characterise the dominant formative processes over the fans. The stream flow sediments dominate the Rait-Rihlu fans, whereas the debris flow sediments dominate the Kangra and Palampur fans. The fan sequences are also marked by the formation of strongly developed paleosols on loess (L1–L3 loess paleosols) and weakly developed paleosols on fluvial deposits in response to the tectonics and climate change in NW Himalayas.     

Holocene paleosols and colluvial sediments in Northeast Tibet (Qinghai Province,China): Properties,dating and paleoenvironmental implications

Colluvial deposits consisting of silts and loams were detected in several climatologically different areas of NE Tibet (3200–3700 m a.s.l.). Layering, distinct organic content and low content of coarse matter as well as location in the relief revealed an origin from low-energy slope erosion (hillwash). Underlying and intercalated paleosols were classified as Chernozems, Phaeozems, Regosols and Fluvisols. Fifteen radiocarbon datings predominant on charcoal from both colluvial layers and paleosols yielded ages between 8988 ± 66 and 3512 ± 56 uncal BP. Natural or anthropogenic factors could have been the triggers of the erosional processes derived. It remains unclear which reason was mainly responsible, due to controversial paleoclimatic and geomorphic records as well as insufficient archaeological knowledge from this region. Determinations of charcoal and fossil wood revealed the Holocene occurrence of tree species (spruce, juniper) for areas which nowadays have no trees or only few forest islands. Thus large areas of NE Tibet which are at present steppes and alpine pastures were forested in the past.     

Kaolinitic paleosols in the south west of the Iberian Peninsula (Sierra Morena region, Spain). Paleoenvironmental implications

This paper studies the physical and chemical characteristics of eight different soil profiles with paleohorizons rich in kaolinites and developed on different lithologies along the southern border of the Hercinian Iberian peninsula (Sierra Morena region).The paleohorizons of four of these soils are defined by low pH levels, desaturation of the exchange complex and proportions of kaolinite of over 75%; these characteristics are associated with subtropical pedogenic conditions during the Pliocene period.A further two soil profiles are contemporary and defined by the following features: they occupy depression areas, the clay fraction is dominated by kaolinites and smectites, the exchange complex is saturated and the pH is above neutral values.The last two soil profiles are developed on Pliocene continental deposits and have more moderate pedogenic features, their kaolinite levels are around 50% and their evolution is associated with shorter periods of exposure to these subtropical alteration conditions.     

Comparative characterization of microbial communities in kurgans,paleosols buried under them,and background surface soils in the steppe zone of the Lower Volga region

A comparative analysis of the state of microbial communities in kurgans, paleosols buried under them, and background surface soils in the dry steppe zone of the Lower Volga region has been performed. It is shown that the population density of microorganisms of various trophic groups in the kurgans is an order of magnitude lower than that in the A1 horizon of the corresponding buried paleosols and background surface soils within the areas of chestnut, light chestnut, and solonetzic soils. The respiration activity of the microbial communities in the upper layer of the kurgans is comparable with that in the A1 horizons of the background surface soils; it decreases in the deeper layers of the kurgans. In the A1 horizon of the buried paleosols, the respiration activity is approximately the same as in the deep layers of the kurgans. In the buried paleosols, the spatial variability in the numbers of soil microorganisms is approximately the same or somewhat higher than that in the background surface soils. The spatial variability in the respiration activity of the buried paleosols is two to four times higher than that in the background surface soils.     

Snow chemistry in the central Sierra Nevada,California

Precipitation and snowpack basal outflow event samples were analyzed for pH and NO and SO₄ concentrations at a site near Lake Tahoe, California. TJ seasonal minimum pH from basal outflow was synchronous with a rain-on-snow event in 1984. Outflow pH reflected the low ionic concentrations of precipitation at the site. There was no evidence for a pulse of acidified meltwater at this site either during a mid-February melt induced by high air temperatures in 1985 or during 1984 or 1985 main spring melt periods. During the mid-February 1985 melt, however, an alkalinity pulse occurred in basal outflow.     

Spatial structure of multispecies distributions in southern California, USA

Analysis of the spatial distribution of all species of conservation importance within a region is necessary to augment reserve selection strategies and habitat management in biodiversity conservation. In this study, we analyzed the spatial aggregation, spatial association, and vegetation types of point occurrence data collected from museum and herbaria records for rare, special concern, threatened, and endangered species of plants, reptiles, mammals, and birds in western Riverside County in southern California, USA. All taxa showed clumped distributions, with aggregation evident below 14 km for plants, 12 km for reptiles, 2 km for mammals, and 10 km for birds. In addition, all combinations of the different species groups showed high positive spatial association. The Santa Rosa Plateau exhibited the highest number of rare, special concern, threatened, and endangered species, and shrubland (coastal sage and chaparral) was the vegetation type inhabited by the most species. Local land use planning, zoning and reserve design should consider the spatial aggregation within and between species to determine the appropriate scale for conservation planning. The higher spatial association between species groups in this study may indicate interdependence between different species groups or shared habitat requirements. It is important to maintain diverse communities due to potential interdependence. The results of the study indicate that concentrating preservation efforts on areas with the highest number of species of concern and the restoration of native shrublands are the most appropriate actions for multiple species habitat conservation in this area.     

Restoring plant cover on high-elevation gravel areas, Sequoia National Park, California

Our objective was to learn whether Carex exserta sod plugs could be successfully transplanted as a technique for restoring plant cover on high-elevation gravel areas of the southern Sierra Nevada. Our study area was Siberian Outpost in Sequoia National Park, California. The plugs (either 1·9 cm or 5·1 cm in diameter and 10-cm deep) were transplanted in September 1981 and 1982 and without papier-mâché pots and fertilizer. The most promising treatment (52% survival after four years) was to transplant large-diameter sod plugs unpotted and unfertilized. Water appears to be the main factor limiting existing plant cover at Siberian Outpost. Nevertheless, plants present in the gravel could not effectively use fertilizer, and some species were reduced by fertilization.     

Silicon,aluminum, and oxalic acid interactions in two California forest soils

Abstract

The release of solid‐phase soil aluminum (Al) from two soils was studied under acidic conditions and also in the presence of monosilicic acid. The soils support mixed‐conifer forests in the mid‐elevation Western Sierra Nevada in northern California, but differ in their state of development and mineralogy as shown by Al, iron (Fe), and silicon (Si) concentrations. The pyrophosphate‐extractable Al (Al_p) pool, which was a main source of released Al, decreased after a two‐month leaching with nitric (HNO₃) or oxalic (HO₂C‐CO₂H) acids. Addition of monosilicic acid (SiO₂.XH₂O) to the acid extractants resulted in a further decrease of Al. Solution monosilicic acid was removed from solution by sorption on Fe oxides/hydroxides in the soil with the higher dithionite‐extractable Fe pool. In the less developed soil with lower pedogenic Fe, the formation of short‐range‐ordered aluminosilicates, even in the presence of a strong Al chelator, was responsible for the removal of a portion of the monosilicic acid from solution. Pedogenic Fe inhibited the formation of short‐range‐ordered aluminosilicates more than the presence of a strong Al chelator. Both the solution phase and surface reactions are important in the pedogenic formation of alumino‐silicate minerals.     

Elemental concentrations in fishes from the Salton Sea,Southeastern California

The Salton Sea is a 93 000 ha saline lake fed by drainage water from more than 283 000 ha of irrigated lands in the Imperial and Coachella valleys of California. A total of 21 composite samples of four recreationally important fish species — bairdiella (Bairdiella icistia), orangemouth corvina (Cynoscion xanthulus), sargo (Anisotremus davidsoni), and Mozambique tilapia (Tilapia mossambica) —collected there were analyzed for 14 elements. Twelve of these elements were detected in one or more of the samples: As, B, Co, Cu, Fe, Hg, Mo, Ni, Pb, Se, V, and Zn. Cadmium and Tl were not detected. The ranges in concentrations of elements in the skinless fillets of bairdiella, corvina, and sargo, and in whole bodies of all four fishes were comparable to levels that are typically measured in saltwater fishes. Only Se concentrations were elevated (as much as 14 µg g^?1 dry weight in both fillets and whole bodies) in this series of samples. Elevated concentrations of Se have already led to public health advisories concerning the consumption of fish and might eventually cause the demise of fish populations from toxic effects.