The paleolimnology of Haynes Lake, Oak Ridges Moraine, Ontario, Canada: documenting anthropogenic and climatic disturbances     

Melissa A. Watchorn  Paul B. Hamilton  R. Timothy Patterson 《Environmental Earth Sciences》2013,68(7):1823-1834

Haynes Lake is a small kettle lake located on the Oak Ridges Moraine, and is within the Greater metropolitan area of Toronto, Ontario; Canada’s most populous region. Lake sedimentation, flux rates, diatoms and thecamoebians extracted from a benthic core were used as biological proxies to evaluate changes in water quality through time as a function of anthropogenic activity and changing climate. There were two periods of disturbance to the Haynes Lake ecosystem from ca 8,500 years before present (YBP) through to ca A.D. 2003, which were significant enough to cause changes in lake sedimentation, the diatom flora, and thecamoebian fauna. The first disturbance was concomitant with the decline in global temperatures following the Hypsithermal Climate Optimum (ca. 4,700 YBP). The most significant disruption to Haynes Lake over the last 8,500 years, however, was the settlement of Europeans and subsequent urban development (ca. A.D. 1875), including the construction of a road immediately adjacent to the lake. Anthropogenic disturbance of inorganic clays in the recent paleosediment record (<5 cm) is indicative of more recent eutrophication events.  相似文献   

Observational constraints on the identification and distribution of chaotic terrain on icy satellites     

C.D. Neish  L.M. Prockter  G.W. Patterson 《Icarus》2012,221(1):72-79

We outline the observational constraints required to identify chaos regions on Europa. Large incidence angle, rather than high resolution, appears to be the primary observational requirement for identifying chaos. At incidence angles >70°, chaos can be identified on Europa at image resolutions as low as 1.5 km/pixel. Similar images obtained at moderate or low incidence angles (<50°) require image resolutions upwards of ～250 m/pixel to identify chaos. If global images of Europa can be acquired at high incidence angles, the majority of its chaotic terrain can be identified, helping to constrain models of chaos formation and distribution. Furthermore, our results indicate that the areal coverage of chaos may be more uncertain than previously reported, representing as little as 10% or as much as 50% of the non-polar regions of Europa. These guidelines will aid in the development of optical instruments for future Europa missions, as well as other icy bodies, such as Triton.  相似文献   

Carbon isotopes of marl and lake sediment organic matter reflect terrestrial landscape change during the late Glacial and early Holocene (16,800 to 5,540 cal yr B.P.): a multiproxy study of lacustrine sediments at Lough Inchiquin,western Ireland   总被引：1，自引：0，他引：1  

Aaron F. Diefendorf  William P. Patterson  Chris Holmden  Henry T. Mullins 《Journal of Paleolimnology》2008,39(1):101-115

A 7.6-m lake sediment core from a marl lake, Lough Inchiquin, records variation in landscape evolution from 16,800 cal yrs B.P. to 5,540 cal yrs B.P. We observe significant variations (up to 12‰) in δ ¹³C_org and δ ¹³C_calcite values that are interpreted to reflect secular changes in lake water δ ¹³C_DIC values that result from a regional landscape transition from barren limestone bedrock to a forested ecosystem. Lake water δ ¹³C_DIC values are therefore influenced by two isotopically distinct sources of carbon: terrestrial organic material (−27.1 to −31.2‰VPDB) via oxidized soil organic matter and weathered limestone bedrock (+3.4‰VPDB). Isotope excursions in lacustrine sediment records are forced not only by changes in productivity but also by changes in the terrestrial environment. This has profound implications for the interpretation of paleoclimate records derived from lacustrine sediment and suggests that selection of appropriate lakes can provide records of terrestrial change where other related records are not available.  相似文献   

Diatoms and pollen as indicators of water quality and land-use change: a case study from the Oak Ridges Moraine,Southern Ontario,Canada     

Melissa?A.?WatchornEmail author  Paul?B.?Hamilton  Thane?W.?Anderson  Helen?M.?Roe  R.?Timothy?Patterson 《Journal of Paleolimnology》2008,39(4):491-509

Swan Lake is a small kettle lake located on the Oak Ridges Moraine; a moraine that is recognized as an important source of ground water for the nearby and rapidly expanding Greater Toronto Area. A paleolimnological reconstruction using pollen and diatoms from the lake sediments showed significant changes in biological community composition through the last ∼400 years. Alterations in the diatom and pollen assemblages were most dramatic ca. A.D. 1850, correlating with the highest sediment flux in the lake between the period ca. A.D. 1850 and A.D. 1870. These changes were directly linked to regional deforestation and agricultural activities associated with European settlement. The pollen record from ca. A.D. 1850 to present day indicated that tree species (e.g. Pinus spp., Tsuga canadensis) were declining, while grass (Poaceae) and invasive species (e.g. Ambrosia) were increasing. Around A.D. 1850, the diatom flora changed from an assemblage dominated by large, benthic species (e.g. Sellaphora pupula, Pinnularia cf. maior, and Stauroneis phoenicenteron) to an assemblage characterized by smaller, tychoplanktonic (e.g. Fragilaria tenera, Staurosirella pinnata) and epiphytic (e.g. Achnanthidium minutissimum, Rossithidium linearis) taxa. This diatom community change supports the intermediate disturbance hypothesis which predicts a high level of diversity and richness following an intermediate to intense disturbance of short duration. Phosphorus concentrations in Swan Lake were inferred using a diatom-based regional calibration model, and the results indicated marked changes in lake water chemistry through time (from below detection limits before land clearance and settlement to 19.3 μg l⁻¹ in the current sediments), which were concurrent with episodes of regional deforestation and land-use change. Although the sediment and biological records indicate that the lake ecology has stabilized over the last 30–50 years, paleolimnological records show that the water quality and biology of Swan Lake has changed dramatically and not returned to pre-settlement conditions. Swan Lake presents a detailed record of the impact created by deforestation and urban development with a population of <50 individuals per km². Detailed paleolimnological studies like Swan Lake, in tandem with global human footprint studies, can create realistic estimates of land-use impacts at the global scale.  相似文献   

A Field Test of Electromigration as a Method for Remediating Sulfate from Shallow Ground Water     

Charles G. Patterson  Donald D. Runnells 《Ground Water Monitoring & Remediation》1996,16(4):63-68

Eloctromigraiion offers a potential tool for remediating ground water contaminated with highly soluble components, such as Na⁺, Cl, NO₃ and SO₄⁻. A field experiment was designed to lest the efficacy of electromigration for preconcontrating dissolved SO₄² in ground water associated with a fossil-fuel power plant. Two shallow wells, 25 feel apart (one 25 feel deep, the other 47 feet deep), were constructed in the upper portion of an unconfined alluvial aquifer. The wells were constructed with a double-wall design, with an outer casing of 4-inch PVC and an inner lube of 2-inch FVC; both were fully slotted (0.01 inch). Electrodes were constructed by wrapping the inner lulling with a 100-foot length of rare-earth metal oxide/copper wire. An electrical potential of 10.65 volts DC Was applied, and tests were run for periods of 12, 44, and 216 hours. Results showed large changes in the pH from the initial pH of ground water of about 7.5 to values of approximately 2 and 12 at the anode and cathode, respectively. Despite the fact that the test conditions were far from ideal, dissolved SO₄^2-; was significantly concentrated at the anode. Over a period of approximately nine days, the concentration of SO₄^2- at the anode reached what appeared to he a steady-state value of 2200 mg/L. compared lo the initial value in ground water of approximately 1150 mg/L. The results of this field lest should encourage further investigation of electromigration as a tool in the remediation of contaminated ground water.  相似文献   

Data Elements for Reporting Water-Quality Results     

Charles Job  Glenn Patterson 《Ground Water Monitoring & Remediation》2001,21(4):36-38

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Changes of lead and barium with time in California off-shore basin sediments     

Amy No  Clair C. Patterson 《Geochimica et cosmochimica acta》1982,46(11):2307-2321

During ancient times the natural deposition fluxes of lead which can be leached with dilute acid from sediments in Santa Barbara, Santa Monica and San Pedro basins offshore from the Los Angeles Urban complex, were about 0.7, 0.1 and 0.2 μg Pb/cm² yr respectively. Since there was little difference in biological productivity in surface waters of these basins, it is proposed that clay is a major transport vehicle for sequestered soluble lead, which then explains why the lead deposition flux within the Santa Barbara basin was so much larger compared to the other basins. The fluxes of silicate mud in the basins in ancient times were about 92, 19 and 30 mg/cm² yr in Santa Barbara, Santa Monica and San Pedro basins respectively. Today deposition fluxes of acid soluble lead within these three basins are 3- to 9-fold greater, being about 2.1, 1.1 and 1.8 μg Pb/cm² yr respectively, partly in the form of directly deposited large sewage particles, which account for none, $\text{2}\text{3}$ and $\text{3}\text{4}$ of the total industrial lead deposition fluxes in the respective basins. Concentrations of leachable lead in varve dated sediment layers increase with time and isotopic compositions of these leads change in accordance with corresponding known changes of isotopic compositions of industrial lead in the Los Angeles atmosphere. Lead remaining in acid leached sediment residues originates from igneous and clay minerals, exhibiting no change in concentration or isotopic composition since pre-industrial times.Deposition fluxes of total barium in sediments among the three basins were proportional to mass deposition fluxes before 1950 in the same manner as for lead. Afterwards, there are barium concentration maxima with time in both Santa Monica and San Pedro Basin sediments which are attributable to industrial sewage rather than to episodic erosion from barium-rich sedimentary evaporite strata exposed locally along the shore. An increase of barium concentrations in present day Santa Barbara basin sediments may reflect dispersal of barium-rich drilling mud from local drilling operations.  相似文献   

Lead concentrations in the northeast Pacific: evidence for global anthropogenic perturbations     

Bernhard K. Schaule  Clair C. Patterson 《Earth and Planetary Science Letters》1981,54(1):97-116

Lead concentrations were determined by isotope dilution mass spectrometry in 34 surface- and deep-water samples collected in the northeast Pacific between Hawaii and California and off the California coast using a deep-water sampler protected against fouling by contamination from the ship and hydrowire. Measured concentrations lie more than one order of magnitude below previously published open ocean values and they show that in most cases 90% or more of the total lead is in a dissolved form. Lead concentrations are about 10-fold higher in surface and thermocline waters than in deep waters; values drop as low as 1 ng/kg (5 pmol/kg) below 3500 m depth. Lead profiles thus appear different compared to those of most trace metals, which show enrichment in deep waters compared to surface concentrations. Lead concentrations in surface waters increase from 5 to 15 ng/kg (25 to 75 pmol/kg) along a transect starting from a location 200 km off the California coast and continuing towards the center of the North Pacific Gyre. This increase is congruent with that observed for²¹⁰Pb concentrations in the same waters sampled at the same time.Lead is supplied to the open North Pacific largely from the atmosphere, at a rate of about 60 ng/cm² yr, which exceeds the prehistoric oceanic output flux of authigenic lead recorded in pelagic sediments about tenfold. This excess originates from emissions from smelters and combustion of leaded gasoline, overwhelming natural lead inputs that entered the ocean during prehistoric time probably largely through rivers. Vertical lead concentration profiles below the surface mixed layer are probably not in steady state. There, concentrations must be increasing in response to the increase of anthropogenic inputs because the estimated lead residence times are more than 20 years in the thermocline and about 80 years in deep waters. Based on an estimated 10-fold input and concentration increase since the mid-eighteenth century in the surface mixed layer in the central northeast Pacific, it is calculated that the 10 ng/kg average concentration between 100 and 900 m is 2 to 5 times larger, and the 1.8 ng/kg average concentration between 900 and 5000 m depth is about 2 times larger than it was in the mid-eighteenth century. Profiles of lead concentrations in the North Atlantic are expected to be shifted generally to larger values by a factor of 2 to 3 compared to those in the North Pacific because of the effects of greater industrial lead contamination, while lead concentration profiles in the South Pacific are expected to be shifted generally to lower values compared to the North Pacific by about this same factor because of the effects of lesser industrial lead contamination.  相似文献   

Improved techniques for studies of mass balances and fractionations among families of metals within terrestrial ecosystems     

Robert W Elias  Todd K Hinkley  Yoshimitsu Hirao  Clair C Patterson 《Geochimica et cosmochimica acta》1976,40(6):583-587

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Elevation models for reproducible evaluation of terrain representation     

Patrick J. Kennelly  Tom Patterson  Daniel P. Huffman    Sarah Bell 《制图学和地理信息科学》2021,48(1):63-77

ABSTRACT

This paper proposes elevation models to promote, evaluate, and compare various terrain representation techniques. Our goal is to increase the reproducibility of terrain rendering algorithms and techniques across different scales and landscapes. We introduce elevation models of varying terrain types, available to the user at no cost, with minimal common data imperfections such as missing data values, resampling artifacts, and seams. Three multiscale elevation models are available, each consisting of a set of elevation grids, centered on the same geographic location, with increasing cell sizes and spatial extents. We also propose a collection of single-scale elevation models of archetypal landforms including folded ridges, a braided riverbed, active and stabilized sand dunes, and a volcanic caldera. An inventory of 78 publications with a total of 155 renderings illustrating terrain visualization techniques guided the selection of landform types in the elevation models. The benefits of using the proposed elevation models include straightforward comparison of terrain representation methods across different publications and better documentation of the source data, which increases the reproducibility of terrain representations.  相似文献