Holocene vegetation and climate dynamics of the boreal alpine ecotone of northwestern Fennoscandia     

Christin Jensen  Karl‐Dag Vorren 《第四纪科学杂志》2008,23(8):719-743

Climate change with respect to summer temperature throughout the Holocene is inferred from oscillations in the local Pinus sylvestris, Alnus incana and Betula pubescens forest‐lines, as recorded by fossil pollen and plant macrofossils in lake sediments at four altitudinal levels. Mt Skrubben (848 m a.s.l.), in Dividalen, was deglaciated down to below 280 m a.s.l. during 10 800–10 300 cal. yr BP. Betula pubescens established 10100 cal. yr BP at 280 m a.s.l. and expanded up to near the summit during the next 700 years. Birch woodland prevailed on the mountain plateau until 3300 cal. yr BP. Local Pinus sylvestris stands are recorded up to 400 m a.s.l. at 8450 cal. yr BP and >548 m a.s.l. about 8160 cal. yr BP. Alnus incana expanded from 400 to nearly 790 m a.s.l. during the period 7900–7600 cal. yr BP. The maximum forest distribution lasted until ca. 6000 cal. yr BP. Marked climatic deteriorations caused lowering of the forest‐lines around 4600 and 3000 cal. yr BP. Reconstruction of the summer temperature indicated mean July temperatures at 400 m a.s.l. of 1.5–3°C above the present during the period of maximum forest expansion, whereas >3°C above the present temperature at 548 m a.s.l. This is in accordance with other regional temperature reconstructions from northern Europe. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献   

PCB contamination from sampling equipment and packaging     

Malin Andersson  Rolf Tore Ottesen  Morten Jartun  Ola Eggen  Ann-Christine Enqvist 《Applied Geochemistry》2012

Work reported in this paper suggests that there are cases of contamination of soil and water samples by polychlorinated biphenyls (PCB) from paper and plastic packaging. Soil samples, which have been stored in paper bags for more than 20 years, share a similar congener distribution as the bags. Analyses showed a predominance of light congeners. PCB-analyses of water also indicate that water samples could be contaminated by plastic packaging. All analytical results of solid material packaging, as well as soil stored in the packaging, show a high relative amount of light weight PCB congeners. The paper bags that were analysed are made of strong paper and very popular among geochemists because of their watertight quality. These paper bags were manufactured more than 20 years ago. The plastic packaging that was analysed was produced in 1997 and 2008. The analyses of plastic and paper show that the raw material that has been used in the production at different times contains a wide concentration range of PCB. Re-sealable plastic bags, which contained the highest levels of PCB of the plastic material, are used by researchers world-wide as sampling bags for soils and sediments. This paper raises an important issue that packaging may potentially contaminate the samples that they hold.  相似文献   

Flood disaster in Taihu Basin,China: causal chain and policy option analyses     

Wang Liang  Cai Yongli  Chen Hongquan  Dag Daler  Zhao Jingmin  Yang Juan 《Environmental Earth Sciences》2011,63(5):1119-1124

Taihu Lake is at the densely populated region of the eastern coast of China. Taihu Basin is one of the most developed regions of China. The frequency of flood disaster in Taihu Basin has been increasing in the recent years, resulting in more drowned areas and economic loss. It is shown that flood disaster is the most serious problems in Taihu Lake and Taihu Basin. Mitigation of flood problems and return to sustainability has now been given high attention and are prioritized in the Chinese national policies. This paper describes the state of the flood disaster in the Taihu Basin, examines the root causes for flood disaster, demonstrates by examples how these analyses known as transboundary diagnostic analysis can be used to develop policy options that can help predict and reduce the flood disaster based on past and current measures and policy.  相似文献   

Drag force on a vegetation field due to long-crested and short-crested nonlinear random waves     

Dag Myrhaug  Lars Erik Holmedal 《Coastal Engineering》2011

This paper provides a practical method for estimating the drag force on a vegetation field exposed to long-crested (2D) and short-crested (3D) nonlinear random waves. This is achieved by using a simple drag formula together with an empirical drag coefficient given by Mendez et al. (1999), in conjunction with a stochastic approach. Here the waves are assumed to be a stationary narrow-band random process. Effects of nonlinear waves are included by adopting the Forristall (2000) wave crest height distribution representing both 2D and 3D random waves.  相似文献   

Dynamic Versus flexural Controls of Late Cretaceous Western Interior Basin, USA     

LIU Shaofeng  Dag NUMMEDAL  LIU Lijun 《《地质学报》英文版》2013,87(Z1):572-573

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Five centuries of Stockholm winter/spring temperatures reconstructed from documentary evidence and instrumental observations   总被引：1，自引：0，他引：1  

Lotta Leijonhufvud  Rob Wilson  Anders Moberg  Johan Söderberg  Dag Retsö  Ulrica Söderlind 《Climatic change》2010,101(1-2):109-141

Historical documentary sources, reflecting different port activities in Stockholm, are utilised to derive a 500-year winter/spring temperature reconstruction for the region. These documentary sources reflect sea ice conditions in the harbour inlet and those series that overlap with the instrumental data correlate well with winter/spring temperatures. By refining dendroclimatological methods, the time-series were composited to a mean series and calibrated (1756–1841; r ²?=?66%) against Stockholm January–April temperatures. Strong verification was confirmed (1842–1892; r ²?=?60%; RE/CE?=?0.55). By including the instrumental data, the quantified (QUAN) reconstruction indicates that recent two decades have been the warmest period for the last 500 years. Coldest conditions occurred during the 16th/17th and early 19th centuries. An independent qualitative (QUAL) historical index was also derived for the Stockholm region. Comparison between QUAN and QUAL shows good coherence at inter-annual time-scales, but QUAL distinctly appears to lack low frequency information. Comparison is also made to other winter temperature based annually resolved records for the Baltic region. Between proxy coherence is generally good although it decreases going back in time with the 1500–1550 period being the weakest period—possibly reflecting data quality issues in the different reconstructions.  相似文献   

Composition and properties of glacigenic sediments in the southwestern Barents Sea     

Joar Sættem  Leif Rise  Dag Arne Westgaard 《Marine Georesources & Geotechnology》2013,31(3-4):229-255

Abstract

The composition and properties of glacigenic sediments in the southwestern Barents Sea are described based on data from 33 shallow boreholes (< 143 m below seabed) and 11 seabed cores (<4.2m below seabed). The cores are tied into a regional seismostratigraphic framework, illustrating the relationships between different boreholes.

A massive, muddy diamicton (silty, sandy clay with scattered gravel) is found in nearly all cores. Average clay content (<2 pm) of this lithology is about 38%, but varies between about 25% and 50%. Short intervals of finely laminated, waterlain sediments or gravelly sand are cored in a few occasions. A high content of sand and gravel in the cores from near the Norwegian coast shows an influence of sediment input from the mainland, while material eroded from sedimentary rocks dominates farther offshore.

The data presented on physical properties include undisturbed and remolded undrained shear strength, natural water content, bulk density, compressional sound velocity (P waves), Atterberg consistency limits, effective preconsolidation pressure, and consolidation coefficient.

Prediction of overconsolidation from seismic mapping of erosional surfaces is confirmed by the borehole cores. High compaction is found both in Weichselian and older deposits, with a general increase in compaction toward the east as well as toward shallower water. Cores that are “underconsolidated” at their present burial depth are also reported.

The average compressional sound velocity is about 1780 m/s for the borehole cores, 1550 m/s for the seabed cores, and increases with increasing shear strength and consolidation. Both horizontal and vertical sound velocities are measured in several cores, and although the data have a considerable scatter, a slightly aniso‐tropic sound velocity is indicated.  相似文献   

Book reviews     

W. Krumbein  U. Förstner  E. Plate  John Lewin  Georg Matthess  E. Löffler  Dag Nummedal  A. Zaporozec  G. Kunkel  Pierre Biays  Karl W. Butzer  J. Humlum  Gunnar Alexandersson  W. R. Stanley  Ernst Löffler  Åke Hillefors  Yrjö Vasari  E. M. Yates 《GeoJournal》1979,3(5):499-508

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Heat generation versus depth of crystallization for Norwegian monzonitic rocks     

Dag E. Ormaasen  Gunnar Raade 《Earth and Planetary Science Letters》1978,39(1):145-150

Thorium, U and K analyses by γ-ray spectrometry of monzonitic intrusives from Lofoten-Vesterålen (ca. 1800 m.y.), Bjerkreim-Sogndal (ca. 1000 m.y.) and the Oslo region (ca. 275 m.y.) are used to calculate values of radioactive heat generation. A strong negative correlation between heat generation and depth of crystallization is demonstrated, indicating that the chemical zoning of the continental crust with respect to Th and U is of a rather regional and regular character, and was probably firmly established at least 1800 m.y. ago. The K contents, in contrast to Th and U, show an increase with depths of crystallization for these rocks. This may be explained by considerations of the pressure dependence of the partition coefficients for these elements between minerals and magma, and the importance of a fluid phase as a transport medium for the incompatible elements Th and U. A positive correlation between K content and age of intrusion is discussed on a tentative basis.  相似文献   

Key site variables governing the functional characteristics of Dissolved Natural Organic Matter (DNOM) in Nordic forested catchments   总被引：1，自引：0，他引：1  

Rolf D. Vogt  Jarkko Akkanen  Dag Olav Andersen  Rainer Brüggemann  Bimal Chatterjee  Egil Gjessing  Jussi V. K. Kukkonen  Håkon E. Larsen  Jörg Luster  Andrea Paul  Stephan Pflugmacher  Mike Starr  Christian E. W. Steinberg  Philippe Schmitt-Kopplin  Ádám Zsolnay 《Aquatic Sciences - Research Across Boundaries》2004,66(2):195-210

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