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排序方式: 共有112条查询结果,搜索用时 15 毫秒
1.
A reconstruction of the palaeohydrological conditions of a flood‐plain: a multi‐proxy study from the Grabia River valley mire,central Poland 下载免费PDF全文
Dominik Pawłowski Grzegorz Kowalewski Krystyna Milecka Mateusz Płóciennik Michał Woszczyk Tomasz Zieliński Daniel Okupny Wojciech Włodarski Jacek Forysiak 《Boreas: An International Journal of Quaternary Research》2015,44(3):543-562
This study investigated the Grabia River valley mire in central Poland to reconstruct its palaeoenvironmental conditions from the Younger Dryas to the present. We analysed sedimentological, biological and geochemical data from the palaeo‐oxbow lake and valley mire to identify the principal hydrological trends, especially episodes of high water level. During the Lateglacial and Holocene, the Grabia River had a meandering channel, and its hydraulic parameters and the channel dimensions changed in response to climatic oscillations and vegetation development. We identified phases of high flood intensity and high groundwater level that correlate with regional and supraregional climatic events. The frequency and timing of palaeohydroclimatic oscillations show strong similarities to records from other sites in Poland and the rest of Europe. We show that various analytical methods, namely, pollen, plant macrofossils, Cladocera, Chironomidae, sedimentological, geochemical and radiocarbon data, can be effective tools for reconstructing past hydroclimatic changes in palaeo‐oxbow lakes and investigating the effects of past climate changes on river environments. The high sensitivity of the biota, especially Cladocera, to changes in water level permits the reconstruction of palaeoecological changes, especially flood episodes that occurred in the river valley. In particular, the increase in the proportion of sediment‐associated Cladocera and pelagic taxa was closely correlated with floods. Through comparisons with the palaeobiological data, geochemical data allowed the identification of humid phases within the fen associated with a rising groundwater table, direct fluvial activity (floods) and alluvial deposition. We also discuss the limitations of palaeohydrological reconstructions based on these proxies, especially on fossil aquatic invertebrates. 相似文献
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Y. D. Zakharov M. Horacek Y. Shigeta A. M. Popov L. G. Bondarenko 《Stratigraphy and Geological Correlation》2018,26(5):534-551
N and C isotopic data are recorded and presented for the first time for the Lower Triassic claystones of Southern Primorye (Abrek Section). Five N isotope intervals and 11 more or less pronounced negative C isotope excursions, likely to reflect instability of the temperature regime and the oceanographic situation in the Early Triassic, are recognized in the section. The most favorable conditions for ammonoid recovery and other marine organisms in the Early Triassic (after the end- Permian ecological crisis) were associated with the late Induan—early Olenekian transgression and probable cooling. 相似文献
4.
Leszek Marynowski Michał Zatoń Bernd R.T. Simoneit Angelika Otto Mariusz O. Jędrysek Cezary Grelowski Slawomir Kurkiewicz 《Applied Geochemistry》2007
The comprehensive biomarker characteristics from previously undescribed Middle Jurassic clays of Poland are presented. The molecular composition of the organic matter (OM) derived from clays of Aalenian to Callovian age has not changed significantly through time. High relative concentrations of many biomarkers typical for terrestrial material suggest a distinct dominance of OM derived from land plants. Increasing concentrations of C29-diaster-13(17)-enes towards the northern part of the basin indicate an increase in terrestrial input. This terrestrial material would have originated from the enhanced transport of organic matter from land situated at the northern bank of the basin, i.e., the Fennoscandian Shield. The organic matter was deposited in an oxic to suboxic environment, as indicated by relatively low concentrations of C33–C35 homohopanes, moderate to high Pr/Ph ratio values, an absence of compounds characteristic for anoxia and water column stratification, such as isorenieratane, aryl isoprenoids and gammacerane, as well as common benthic fauna and burrows. δ18O measurements from calcitic rostra of belemnites suggest that the mean value of the Middle Jurassic sea-water temperature of the Polish Basin was 13.1 °C. It is suggested that this mirrored the temperature of the lower water column because belemnites are considered here to be necto-benthic. The organic matter from the Middle Jurassic basin of Poland is immature. This is clearly indicated by a large concentration of biomarkers with the biogenic configurations, such as ββ-hopanes, hop-13(18)-enes, hop-17(21)-enes, diasterenes and sterenes. The identification of preserved, unaltered biomolecules like ferruginol, 6,7-dehydroferruginol and sugiol in Protopodocarpoxylon wood samples from these sediments present particularly strong evidence for the presence of immature OM in the Middle Jurassic sediments. Moreover, the occurrence of these polar diterpenoids is important due to the fact that they are definitely the oldest known natural products detected in geological samples. 相似文献
5.
A modified counter propagation network model and an extended self-organizing map model have the same three-layer network architecture
while employing slightly different learning rules. Their network architecture comprises an input layer, a Kohonen layer and
an output layer. The neurons between two neighboring layers are fully connected and the neighboring neurons within the Kohonen
layer also have neighborhood connections. The modified counter propagation network model employs the Kohonen algorithm to
train the Kohonen layer while using the Widrow–Hoff rule to train the output layer. However, the extended self-organizing
map model applies a modified Kohonen’s learning rule to train both the Kohonen layer and the output layer. This paper compares
the performances of these two models in supervised classification of remotely sensed data. The training results show that
compared to the extended self-organizing map model, the modified counter propagation model has faster learning speed but larger
output errors. The classification results indicate that the extended self-organizing map model has a faster classification
speed and a much higher classification precision than the modified counter propagation model. 相似文献
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This paper is dedicated to the global correlation of the marine Permian-Triassic boundary layers based on some published and original data on the δ13Corg and δ13Ccarb values obtained for the section along the Suol Creek (Setorym River, southern Verkhoyansk region). The section includes six carbon-isotope intervals readily distinguished in the corresponding curves obtained for several Permian and Triassic reference sections in Eurasia and North America including palleontologically well substantiated sections of central Iran, Kashmir, and South China. This provides grounds for assuming the Permian-Triassic boundary’s position in the Suol Creek section as being close to the carbon-isotope minimum of Interval IV. In the light of new data, the upper part of the Upper Permian Changhsingian Stage in Siberia is proposed to correspond in range to the Otoceras concavum range zone, and the lower substage of the Lower Triassic Induan Stage, to the Tompophiceras pascoei and Wordieoceras decipiens zones. The Otoceras concavum Zone of the Verkhoyansk region in its new understanding is likely correlative with the upper Changhsingian Hypophiceras triviale Zone of Greenland. Carbon-isotope intervals II, III, IV, and V defined in the Permian-Triassic boundary layers of the Verkhoyansk region, which are traceable in several reference sections of Eurasia and North America, evidently coincide with the period of some intensification of the volcanic activity in the initial late Changhsingian and with the first phases of extensive eruption of Siberian trappes in the terminal Changhsingian and initial Induan ages. New data imply the probable survival of some ammonoid species from the superfamily Otoceratoidea after the mass extinction of organisms in the terminal Permian Epoch. 相似文献
8.
In the United States, both scholars and practitioners have repeatedly emphasized the importance of “issue framing” for garnering public support for climate change policy. However, the debate frequently overlooks the importance of counter frames. For every framing attempt by advocates of climate policy, there will be a counter frame by the opponents of climate policy. How do counter frames influence the effectiveness of issue framing as a communication strategy? To answer this question, we report results from a survey experiment on a nationally representative sample of 1000 Americans on clean energy policy, a key policy issue in the public debate on climate change in the United States. Overall, we find that different combinations of positive and negative frames have remarkably little effect on support for clean energy policy. A follow-up on-line survey experiment with a convenience sample of 2000 Americans suggests that the counter frames are responsible for undermining the effects of the original frames. 相似文献
9.
Summary ?The intrusive complex of Monzoni in the western central Dolomites (northern Italy) comprises a suite of pyroxenites, monzogabbros
and monzodiorites with solidus temperatures in excess of 1000 °C which intruded previously unmetamorphosed Permotriassic sediments
at less than 5 km depth. At the eastern intrusive contact an approximately 860 m wide contact aureole is developed in the
carbonate country rocks. The prograde sequence of mineral parageneses in a siliceous dolomite of the Cencenighe member and
in marly limestones of the Val Badia and Cencenighe members of the Lower Triassic Werfen formation indicate peak metamorphic
temperatures in excess of 698 °C at 185 m from the intrusive contact and an outward temperature decrease of approximately
65 °C per 100 m. The high temperatures in the inner aureole caused formation of periclase from the prograde breakdown of dolomite
and formation of melilite and esseneite-rich clinopyroxene.
Present address: Mineralogisch-Petrographisches Institut, Universit?t Basel, Switzerland
Received April 7, 2001; revised version accepted December 6, 2001 相似文献
10.
Michał Siwak 《Astrophysics and Space Science》2005,296(1-4):289-292
In this paper we investigate a sample of contact eclipsing binary systems, which exhibit a large temperature difference (at
least 1000 K) between the components. Considering the effective temperature of the primary star, the systems were divided
into three groups. We applied a Monte Carlo method as a more suitable procedure for the search of the system configurations
previously known as contact binaries with a large temperature difference and with a negligible value of the filling factor.
Using only data presented in the literature, we found that the geometrical configuration of almost all systems from the second
group is near-contact rather than contact. 相似文献