scholarly journals Pollen analysis of the surface samples of bottom sediments in the bay of Gdańsk

2015 ◽  
Vol 31 (2) ◽  
pp. 305-312 ◽  
Author(s):  
K. Lubliner-Mianowska
2022 ◽  
Vol 962 (1) ◽  
pp. 012033
Author(s):  
S A Reshetova

Abstract This article presents the results of the study of the bottom sediments of the meromictic Lake Doroninskoe. For the study, the method of spore-pollen analysis was used. The record showed that during the accumulation of 65 cm of the sediment layer in the Chita-Ingodinskaya depression, pine and larch predominated along the ridges, with steppe and meadow associations in the lower parts of the depression. According to regional correlations, the distribution of light-coniferous-taiga vegetation in Transbaikalia occurred as early as the Middle Holocene, and it did not undergo cardinal changes until modern times. According to these data, sediments may have accumulated during this time period.


1986 ◽  
Vol 21 (3) ◽  
pp. 295-302
Author(s):  
Norman A. Rukavina

Abstract New data on bottom sediments and bathymetry provide a more detailed picture of the physical character of the Upper St. Clair River Channel than was previously available. The data indicate that the channel has a complex erosional mid-section cut in glacial deposits and a steep inshore slope with a veneer of modern sediments. Deposits along the Canadian industrial shoreline consist of a thin wedge of nearshore sediment overlying a stiff glacial clay. Estimated volume of the deposit is 63000 m3; average texture is 63% sand, 32% gravel and 5% silt-clay. Tarry interstitial material occurs at or near the surface in shallow-water cores. Size data from surface samples show two strong modes - a sand mode which is consistent with either local derivation or bedload transport and a gravel mode which appears to be too coarse to be natural sediment and may represent fill.


2008 ◽  
Vol 32 (-1) ◽  
pp. 13-19 ◽  
Author(s):  
Jacek Madeja ◽  
Dariusz Latowski

Too Old AMS Radiocarbon Dates Obtained from Moss Remains from Lake Kwiecko Bottom Sediments (N Poland)The paper presents the results of the AMS radiocarbon dating of moss macrofossils which seem to be too old in the context of palynological data. The lack of agreement between the obtained results of radiocarbon dating and pollen analysis has been discussed. Some possible causes of the discrepancies between the results of radiocarbon dating and palynological dating have been given.


1983 ◽  
Vol 61 (5) ◽  
pp. 1510-1521 ◽  
Author(s):  
Paul Comtois

We have undertaken the analysis of 45 surface samples from the Lanoraie peat bogs (45°58′ N, 73°20′ W), situated in the Saint Lawrence lowlands. A reassessment of the different pollen sources that contribute to the pollen rain is carried out. According to the ecology of the species recovered, two principal classes are recognized; proximal and distal. Each of these classes is subdivided in two subclasses according to their extent. The punctual and local sources compose the proximal class, and the regional and zonal sources compose the distal class. The use of similarity and association indices permits the identification of the different distal sources. Thirty-five percent of the distal species are associated among themselves. We identify three habitats: forest, fields, and bogs. We also observe that pollen analysis recovers only those species that make the dominant strata. The characteristic species of Lanoraie are Quercus sp., Salix sp., and the grasses. The strongest pollen productors are Ambrosia artemisifolia (36%), the grasses (10%), and Pinus strobus (8%). We have also outlined the vegetation communities of the proximal class. These communities are discussed first from the point of view of the associations, then from the point of view of the species. According to their hydric characteristics, the elements of the pollen flora are grouped in three types. This inventory should permit a better interpretation of the pollen analysis results in terms of vegetation succession.


Author(s):  
Amel Hassan Abdallah ◽  
Dafaala Ali Ibrahim

Purpose – The purpose of this paper is to measure the environmental changes, which took place in the study area Musawarat ElSufra and the authors try to find the causes of these changes and establish a comparison of the present and past vegetation of the area. Design/methodology/approach – Present vegetation was investigated using fresh plant materials for pollen analysis. Fossils were taken from the hafir (basin) to study the fossil pollen grains at different soil depths. Soil surface samples were taken to analyze the chemical and physical properties of the soil. Findings – The pollen analysis of the samples taken from the hafir (basin) of Musawarat reveals that there are 21 species belonging to 16 families. The dominant families were Cyperaceae, Commelinaceae, Mimosaceae and Amaranthaceae. Originality/value – Comparison of past and present vegetation reveal the causes of environmental change and insure sustainable development in arid region.


Author(s):  
Elvira A. Zinnatova, Larisa A. Frolova ◽  
Larisa A. Frolova

The Northern lakes are good objects for paleoclimatic reconstructions. One of the sources of information about changes in the ecosystems of lakes are diatoms. The study of diatom complexes revealed 133 taxa belonging to 49 genera, 24 families, 13 orders and 3 classes in the bottom sediments of the thermokarst lake of the Pechora Delta. Dominated by the Holarctic representatives of benthic and fouling organisms giving preference to the alkaline environmental conditions.


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