Evolution of a periglacial landscape in the Late Devensian: environments and palaeobotany of the Mepal area,Cambridgeshire, England     

R. G. West  R. G. O. Burton  R. Andrew  M. E. Pettit 《第四纪科学杂志》2002,17(1):31-50

The landscape evolution of the Mepal area from Late Devensian Block Fen Terrace times to the beginning of the Flandrian, a period of ca. 8000 radiocarbon years, is reconstructed. Stratigraphy is based on borehole transects and single boreholes, centred on a depression between the Block Fen Terrace and the Isle of Ely. Within the depression is a Devensian late‐glacial sequence, with the Windermere Interstadial represented by radiocarbon‐dated organic sediments. Pollen and plant macroscopic remains of the late‐glacial sediments are analysed. Plant communities with Betula developed in the interstadial. Before and after the interstadial there is much reworked pollen in the inorganic sediments, derived from local pre‐Devensian Pleistocene sediments, including temperate Ipswichian Stage sediments, and from mass‐wasting of the local Jurassic bedrock. Periods of such mass‐movement occur before and after the deposition of the late‐glacial lake sediments. Deposition of aeolian sediment occurs later than the main period of mass movement, but before the Windermere Interstadial. The relationship of the aeolian sediments in time and space to permafrost, indicated by local contraction polygons and cracks, is discussed. Solifluction diverted the flow of the River Great Ouse from a northeast direction in Block Fen Terrace times to a southwest direction as a channel developed to the west of the Chatteris–March ‘island’. This led to a drainage divide in Flandrian times. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献   

Water mass interaction at intermediate depths in the southern Rockall Trough,northeastern North Atlantic     

Jenny E. Ullgren  Martin White 《Deep Sea Research Part I: Oceanographic Research Papers》2010,57(2):248-257

Mooring time series, CTD data, and Argo float data were analysed to investigate some aspects of the circulation at the southern entrance to the Rockall Trough during 2003–2004. The in situ data are used to describe the distribution at intermediate levels of Sub-Arctic Intermediate Water (SAIW) and Mediterranean Water (MW), as well as the temporal variability in the presence of these two water masses. Salty, MW-influenced water was found in the southeastern part of the study area, near the continental slope as far north as Porcupine Bank, consistent with earlier reports. Apart from the main tongue, the distribution of MW is patchy, and MW parcels were found not only adjacent to the slope but also offshore. Further north and west, water at intermediate depths was influenced by the fresher SAIW. Unlike in some earlier studies, SAIW did not extend as far east as the continental shelf. The year-long hydrographic and current time series from a mooring on the western slope of the entrance, at the southern end of Feni Ridge, showed pulses of SAIW influenced water throughout winter and spring. In late spring, the fresh pulses almost completely ceased; throughout summer only a few weak and shortlived fresh anomalies appeared. The weakening of the SAIW signal did not seem to be caused by winter convection, which did not extend to sufficient depth that winter. The relatively weak SAIW presence during most of the study period may be linked to the near neutral state of the NAO index. The warm and saline conditions observed at the southern entrance to Rockall Trough were in agreement with the rising temperatures and salinities found over large parts of the subpolar North Atlantic in the late 1990s and early 2000s.  相似文献   

Heavy metal resistant endophytic fungi isolated from Nypa fruticans in Kuching Wetland National Park     

Choo  Jenny  Sabri  Nuraini Binti Mohd  Tan  Daniel  Mujahid  Aazani  Müller  Moritz 《Ocean Science Journal》2015,50(2):445-453

Heavy metal pollution is an environmental issue globally and the aim of this study was to isolate endophytic fungi from mangrove wetlands of Sarawak to assess and test their ability to grow in the presence of various heavy metals (copper (Cu), zinc (Zn), lead (Pb), and chromium (Cr)). Samples of Nypa fruticans were collected from Kuching Wetland National Park (KWNP) for subsequent endophyte isolation. Ninety-three (93) isolates were obtained and assessed and the most resistant isolates (growing at concentrations up to 1000 ppm) were identified using fungal primers ITS 1 and ITS 4. All of the endophytic fungi were identified to be closely related to Pestalotiopsis sp. and this is to our knowledge the first study reporting the ability of Pestalotiopsis sp. to grow at high concentrations of copper, lead, zinc and chromium. Our results highlight the potential of using endophytic fungi for the treatment of heavy metal pollution, for example as biosorbents.

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Experimental phase equilibria of a Mount St. Helens rhyodacite: a framework for interpreting crystallization paths in degassing silicic magmas     

Jenny M. Riker  Jonathan D. Blundy  Alison C. Rust  Roman E. Botcharnikov  Madeleine C. S. Humphreys 《Contributions to Mineralogy and Petrology》2015,170(1):1-22

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Chironomid‐inferred late‐glacial summer air temperatures from Lough Nadourcan,Co. Donegal,Ireland     

Jenny E. Watson  Stephen J. Brooks  Nicki J. Whitehouse  Paula J. Reimer  H. John B. Birks  Chris Turney 《第四纪科学杂志》2010,25(8):1200-1210

Western Ireland, located adjacent to the North Atlantic, and with a strongly oceanic climate, is potentially sensitive to rapid and extreme climate change. We present the first high‐resolution chironomid‐inferred mean July temperature reconstruction for Ireland, spanning the late‐glacial and early Holocene (LGIT, 15–10 ka BP). The reconstruction suggests an initial rapid warming followed by a short cool phase early in the interstadial. During the interstadial there are oscillations in the inferred temperatures which may relate to Greenland Interstadial events GI‐1a–e. The temperature decrease into the stadial occurs in two stages. This two‐stage drop can also be seen in other late‐glacial chironomid‐inferred temperature records from the British Isles. A stepped rise in temperatures into the Holocene, consistent with present‐day temperatures in Donegal, is inferred. The results show strong similarities with previously published LGIT chironomid‐inferred temperature reconstructions, and with the NGRIP oxygen‐isotope curve, which indicates that the oscillations observed in the NGRIP record are of hemispherical significance. The results also highlight the influence of the North Atlantic on the Irish climate throughout the LGIT. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

Effects of settling organic matter on the bioaccumulation of cadmium and BDE-99 by Baltic Sea benthic invertebrates     

Thorsson MH  Hedman JE  Bradshaw C  Gunnarsson JS  Gilek M 《Marine environmental research》2008,65(3):264-281

Settling organic matter (OM) is the major food source for heterotrophic benthic fauna. The high sorption affinity of many contaminants for OM implies that OM can influence both the distribution and bioavailability of contaminants. Here, we experimentally examine the role of settling OM of various nutritional qualities on the bioaccumulation of cadmium and the flame retardant BDE-99 by three benthic invertebrates; Macoma balthica, Monoporeia affinis and Marenzelleria sp. Contaminants were associated with three types of OM; a microalgae (Tetraselmis spp.), lignin and sediment. Bioaccumulation of Cd was proportional to OM nutritional quality for all three species, and was species-specific in the order Marenzelleria>M. balthica>M. affinis. BDE-99 bioaccumulation was highest in the treatment with the most nutritious OM (Tetraselmis). Consequently, both benthic species composition and the nutritive value of organic matter settling to the seafloor can have a substantial effect on the bioaccumulation of both metals and organic contaminants.  相似文献   

Three-dimensional versus conventional volcanic hazard maps     

Charles A. Preppernau  Bernhard Jenny 《Natural Hazards》2015,78(2):1329-1347

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Invited responses to Yiftachel and Yacobi, Planning a bi-national capital: should Jerusalem remain united? (Geoforum Vol. 33, No. 1, pp. 137-145.)     

Jenny Robinson 《Geoforum》2002,33(3):275

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Identifying Major Stressors: The Essential Precursor to Restoring Cultural Ecosystem Services in a Degraded Estuary     

Jenny Davis  Ian M. Kidd 《Estuaries and Coasts》2012,35(4):1007-1017

Worldwide estuaries have been subject to multiple and escalating anthropogenic impacts which have resulted in the loss of many ecosystem goods and services including: commercial activities, navigation and marine transportation, recreational and landscape values, and flood control and biodiversity support. An example of these losses is provided in an urban-industrial region of an estuary in northern Tasmania, Australia, where excessive silt deposition has resulted in almost complete loss of the channel at low tide. The causes of siltation have long been attributed to poor watershed management and high concentrations of flocculated and suspended sediments transported upstream by asymmetrical tides. However, historical analysis of anthropogenic changes in estuarine and riverine processes revealed different stressors. These included the decrease in the tidal prism and hence regime equilibrium, brought about by channel infilling and draining of tidal wetlands to create dry land for urban and agricultural uses, and the reduction and redirection of freshwater inflows for the generation of hydroelectricity. Watershed sediment loads exerted a relatively minor role in the estuarine equilibrium, which is solely dependent on tidal flows and river discharges for maintenance of stable cross-sectional areas. Sustainable remediation measures include increasing the tidal prism through the restoration of dynamic river flows and reconnection and restoration of tidal wetlands. However, the former will not be achievable without changes in major provisioning services, particularly the use of water to generate hydroelectricity. This study emphasises the importance of identifying stressors as the basis for examining the potential to reduce the trade-offs between the multiple ecosystem services provided by an estuary and its tributaries, particularly between provisioning and cultural ecosystem services, within a rehabilitation context.  相似文献   

Uneven surface moisture as a driver of dune formation on ephemeral lake beds under conditions similar to the present day: A model-based assessment from the Makgadikgadi Basin,northern Botswana     

Jenny Richards  Sallie Burrough  Giles Wiggs  Tiger Hills  David Thomas  Molatlhegi Moseki 《地球表面变化过程与地形》2021,46(15):3078-3095

An association between salt pans or dry lake beds and distinctive crescentic lake-floor sand mounds (1–10 m high, tens to hundreds of metres wide) is commonplace in desert systems. In the Makgadikgadi Basin of northern Botswana, a debate about the formative processes of these landforms has persisted despite numerous morphometric, sedimentary and geochronological analyses, with mound landforms variously inferred to be aeolian dunes, subaqueous dunes, spring mounds or shoreline remnants. We propose a new formative mechanism which draws on the interaction between uneven moisture distribution on the pan surface and mobile aeolian sediments. We use a numerical model (ViSTA), which couples vegetation and aeolian sand transport dynamics, together with optically stimulated luminescence (OSL) dating of a mound in the Makgadikgadi Basin to investigate the feasibility of this ‘sticky mound hypothesis’. We find that under a range of modelled environmental conditions, uneven moisture distribution on the pan surface can lead to the development and stabilization of crescentic aeolian dunes, with these dunes growing upwind from the point of initial deposition, corresponding with the chronological data gained from OSL dating of a mound feature. On removal of this moisture, the modelled dunes erode and dissipate. These findings suggest that the formative mechanism of the mounds could be dependent on the interaction between differential drying of the pan surface and the competence of the aeolian sediment transport system across the pan floor.  相似文献