LMPHP | Publikacje INoZ

• prof. dr hab. Tadeusz Szczypek

Stanowisko: Profesor
Jednostka: Instytut Nauk o Ziemi
Adres: 41-200 Sosnowiec, ul. Będzińska 60
Piętro: XVII
Numer pokoju: 1711
Telefon: (32) 3689 389
E-mail: tadeusz.szczypek@us.edu.pl
Spis publikacji: Spis wg CINiBA
Scopus Author ID: 9240316000

0000-0002-9123-080X

Publikacje z bazy Scopus

2018

Okuniewska-Nowaczyk, I.; Rahmonov, O.; Snytko, V. A.; Szczypek, T.

Palynological Record of the History of Vegetation in the Sandy Areas of Southern Poland Journal Article

In: Geography and Natural Resources, vol. 39, no. 4, pp. 396-402, 2018, ISSN: 18753728, (2).

Abstract | Links | BibTeX

2017

Rahmonov, O.; Szczypek, T.; Niedźwiedź, T.; Myga-Piątek, U.; Rahmonov, M.; Snytko, V. A.

The human impact on the transformation of juniper forest landscape in the western part of the Pamir-Alay range (Tajikistan) Journal Article

In: Environmental Earth Sciences, vol. 76, no. 8, 2017, ISSN: 18666280, (14).

Abstract | Links | BibTeX

@article{2-s2.0-85018524263,

title = {The human impact on the transformation of juniper forest landscape in the western part of the Pamir-Alay range (Tajikistan)},

author = { O. Rahmonov and T. Szczypek and T. Niedźwiedź and U. Myga-Piątek and M. Rahmonov and V.A. Snytko},

url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85018524263&doi=10.1007%2fs12665-017-6643-4&partnerID=40&md5=499ba0452cb9af79f623030d39cef0d5},

doi = {10.1007/s12665-017-6643-4},

issn = {18666280},

year  = {2017},

date = {2017-01-01},

journal = {Environmental Earth Sciences},

volume = {76},

number = {8},

publisher = {Springer Verlag},

abstract = {Detailed analyses were conducted of human impact on juniper forest landscapes occurring within the Zarafshan Range (Pamir-Alay). Juniperus seravschanica and J. semiglobosa belong to forest-forming species in Central Asia. At present, juniper forests all over Tajikistan are seriously threatened as a result of excessive logging and cattle grazing. The aim of this paper is to present juniper forest transformation as a result of human activities as well as the diversity of soil properties in the organic and humus horizons in the altitudinal system of soil zonation. Three groups of phytocoenoses were distinguished: those with a dominant share of Juniperus seravschanica; those with a dominant share of J. semiglobosa; and mixed. Associations with Juniperus seravschanica and J. semiglobosa feature several variants of phytocoenoses with dominant species: Artemisia lehmanniana, A. dracunculus, Eremurus olgae, Festuca sulcata, Ligularia thomsonii, Stipa turkestanica, Thymus seravschanicus, and Ziziphora pamiroalaica. The collected soil samples differ in their granulometric composition. Gravelly cobble fractions >2 mm are dominant; the share of sandy particles <2 mm is much lower (about 10–20%). Fraction 0.5–0.05 attains 35% on average. The Corg content of the soil varied from 0.26 to 11.40% in the humus horizon (A) and from 4.3 to 25% in the organic (O). Similar relationships were reported in the case of Ntot concentration. A clear relationship can be observed between concentrations of Corg and Ntot. Soil pH varied, ranging from very low acidic (pH 5.5) to neutral (pH 8.5). The content of available P varied; high concentrations were noted in organic (O) (40.46–211 mg kg−1) and mixed horizons (OA) (2.61–119 mg kg−1). Maximum accumulations of Pavail (1739.6 mg kg−1) and Ptot (9696 mg kg−1) were observed at a site heavily affected by intense grazing. Concentrations of Mgavail varied from 116 to 964 mg kg−1. Most of the analysed soil profiles lacked an organic horizon; only thin humus occurred. © 2017, The Author(s).},

note = {14},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

Detailed analyses were conducted of human impact on juniper forest landscapes occurring within the Zarafshan Range (Pamir-Alay). Juniperus seravschanica and J. semiglobosa belong to forest-forming species in Central Asia. At present, juniper forests all over Tajikistan are seriously threatened as a result of excessive logging and cattle grazing. The aim of this paper is to present juniper forest transformation as a result of human activities as well as the diversity of soil properties in the organic and humus horizons in the altitudinal system of soil zonation. Three groups of phytocoenoses were distinguished: those with a dominant share of Juniperus seravschanica; those with a dominant share of J. semiglobosa; and mixed. Associations with Juniperus seravschanica and J. semiglobosa feature several variants of phytocoenoses with dominant species: Artemisia lehmanniana, A. dracunculus, Eremurus olgae, Festuca sulcata, Ligularia thomsonii, Stipa turkestanica, Thymus seravschanicus, and Ziziphora pamiroalaica. The collected soil samples differ in their granulometric composition. Gravelly cobble fractions >2 mm are dominant; the share of sandy particles <2 mm is much lower (about 10–20%). Fraction 0.5–0.05 attains 35% on average. The Corg content of the soil varied from 0.26 to 11.40% in the humus horizon (A) and from 4.3 to 25% in the organic (O). Similar relationships were reported in the case of Ntot concentration. A clear relationship can be observed between concentrations of Corg and Ntot. Soil pH varied, ranging from very low acidic (pH 5.5) to neutral (pH 8.5). The content of available P varied; high concentrations were noted in organic (O) (40.46–211 mg kg−1) and mixed horizons (OA) (2.61–119 mg kg−1). Maximum accumulations of Pavail (1739.6 mg kg−1) and Ptot (9696 mg kg−1) were observed at a site heavily affected by intense grazing. Concentrations of Mgavail varied from 116 to 964 mg kg−1. Most of the analysed soil profiles lacked an organic horizon; only thin humus occurred. © 2017, The Author(s).

2016

Rahmonov, O.; Snytko, V. A.; Szczypek, T.

Influence of melioration in natural ecological processes of a small river valley (Poland) Journal Article

In: Geography and Natural Resources, vol. 37, no. 4, pp. 379-384, 2016, ISSN: 18753728, (3).

Abstract | Links | BibTeX

2014

Rahmonov, O.; Holbegov, M.; Szczypek, T.; Snytko, V. A.; Kłys, G.; Rahmonova, M.

The consequences of vegetation degradation under the influence of anthropogenic activity in the territory of the Zarafshan Range (Western Tajikistan) Journal Article

In: Geography and Natural Resources, vol. 35, no. 2, pp. 193-197, 2014, ISSN: 18753728, (7).

Abstract | Links | BibTeX

2013

Rahmonov, O.; Snytko, V. A.; Szczypek, T.; Parusel, T.

Vegetation development on post-industrial territories of the Silesian Upland (Southern Poland) Journal Article

In: Geography and Natural Resources, vol. 34, no. 1, pp. 96-103, 2013, ISSN: 18753728, (12).

Abstract | Links | BibTeX

2011

Rahmonov, O.; Rahmonova, M.; Snytko, V. A.; Szczypek, T.

Anthropogenic disturbance to vegetation on the polygon-transect in the Kulikalon depression (Tajikistan) Journal Article

In: Geography and Natural Resources, vol. 32, no. 4, pp. 386-393, 2011, ISSN: 18753728, (9).

Abstract | Links | BibTeX

2010

Rahmonov, O.; Snytko, V. A.; Szczypek, T.

Anthropogenic changes in landscape of the Krakow-Czestochowa Upland (Southern Poland) Journal Article

In: Geography and Natural Resources, vol. 31, no. 2, pp. 177-182, 2010, ISSN: 18753728, (6).

Abstract | Links | BibTeX

2009

Rahmonov, O.; Snytko, V. A.; Szczypek, T.

Formation of phytogenic hillocks in Southern Poland Journal Article

In: Geography and Natural Resources, vol. 30, no. 4, pp. 399-402, 2009, ISSN: 18753728, (2).

Abstract | Links | BibTeX

Rahmonov, O.; Snytko, V. A.; Szczypek, T.

Phytogenic hillocks as an effect of indirect human activity Journal Article

In: Zeitschrift fur Geomorphologie, vol. 53, no. 3, pp. 359-370, 2009, ISSN: 03728854, (9).

Abstract | Links | BibTeX

@article{2-s2.0-70350284274,

title = {Phytogenic hillocks as an effect of indirect human activity},

author = { O. Rahmonov and V.A. Snytko and T. Szczypek},

url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-70350284274&doi=10.1127%2f0372-8854%2f2009%2f0053-0359&partnerID=40&md5=008e5de4c2aba7f2f908f4f569aac510},

doi = {10.1127/0372-8854/2009/0053-0359},

issn = {03728854},

year  = {2009},

date = {2009-01-01},

journal = {Zeitschrift fur Geomorphologie},

volume = {53},

number = {3},

pages = {359-370},

abstract = {Phytogenic hillocks are landforms typical for areas built of blown sands. They occur in desert areas with hot and dry (desert) climate as well as in sandy areas in moderate humid climate. They are an effect of cooperation of wind with bushy vegetation of specific features. Under natural desert conditions they are created at e. g. participation of tamarisks and they can reach the height of 6-7 m. In moderate climate, e. g. in area of seaside dunes they are formed at participation of other species and reach decidedly smaller heights. They can also originate in areas of blown inland sands, which were uncovered owing to human activity. One of such areas is located in Silesian Upland in southern Poland (so-called Bledow "Desert"), which beginning goes back to the Middle Ages. It is connected with deforestation, mainly for the needs of contemporary lead, silver and zinc metallurgy. Presently this area is covered in result of intentional vegetation introduction as well as by natural vegetation expansion and succession. One of species intensively entering into this area is Salix arenaria. And just at participation of this bushy willow in deflation areas very characteristic phytogenic hillocks of heights reaching up to 1,5 m are here created using more humid clayey insertions of substratum. They are an effect of these bushes covering up, thanks to which this plant spreads and creates larger and larger landforms. In area discussed it is possible to observe different development stages of phytogenic hillocks-from initial through mature to disappearing ones. The oldest from them were started to create in the period 1973-1976, wherefore the youngest-in the years 2000-2002. The age of hills was determined on the base of dendrochronological analysis. These hills have different shapes and heights, which are conditioned by the intensity of aeolian processes. It is possible to state that phytogenic hillocks of so-called Bledow "Desert" are created by natural physicogeographical processes but conditions for their development were prepared by human being. Thus they are the effect of indirect anthropogenic activity. © 2009 Gebrüder Bornraeger.},

note = {9},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

Phytogenic hillocks are landforms typical for areas built of blown sands. They occur in desert areas with hot and dry (desert) climate as well as in sandy areas in moderate humid climate. They are an effect of cooperation of wind with bushy vegetation of specific features. Under natural desert conditions they are created at e. g. participation of tamarisks and they can reach the height of 6-7 m. In moderate climate, e. g. in area of seaside dunes they are formed at participation of other species and reach decidedly smaller heights. They can also originate in areas of blown inland sands, which were uncovered owing to human activity. One of such areas is located in Silesian Upland in southern Poland (so-called Bledow "Desert"), which beginning goes back to the Middle Ages. It is connected with deforestation, mainly for the needs of contemporary lead, silver and zinc metallurgy. Presently this area is covered in result of intentional vegetation introduction as well as by natural vegetation expansion and succession. One of species intensively entering into this area is Salix arenaria. And just at participation of this bushy willow in deflation areas very characteristic phytogenic hillocks of heights reaching up to 1,5 m are here created using more humid clayey insertions of substratum. They are an effect of these bushes covering up, thanks to which this plant spreads and creates larger and larger landforms. In area discussed it is possible to observe different development stages of phytogenic hillocks-from initial through mature to disappearing ones. The oldest from them were started to create in the period 1973-1976, wherefore the youngest-in the years 2000-2002. The age of hills was determined on the base of dendrochronological analysis. These hills have different shapes and heights, which are conditioned by the intensity of aeolian processes. It is possible to state that phytogenic hillocks of so-called Bledow "Desert" are created by natural physicogeographical processes but conditions for their development were prepared by human being. Thus they are the effect of indirect anthropogenic activity. © 2009 Gebrüder Bornraeger.

2008

Dulias, R.; Pełka-Gościniak, J.; Szczypek, T.

Influence of human activity on the development of aeolian processes in the Silesian-Cracow Upland (Poland) Journal Article

In: Zeitschrift fur Geomorphologie, vol. 52, no. SUPPL. 2, pp. 15-33, 2008, ISSN: 03728854, (9).

Abstract | Links | BibTeX

@article{2-s2.0-59849097636,

title = {Influence of human activity on the development of aeolian processes in the Silesian-Cracow Upland (Poland)},

author = { R. Dulias and J. Pełka-Gościniak and T. Szczypek},

url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-59849097636&doi=10.1127%2f0372-8854%2f2008%2f0052S2-0015&partnerID=40&md5=188ff3d14ed57b57220c2cdd73347c70},

doi = {10.1127/0372-8854/2008/0052S2-0015},

issn = {03728854},

year  = {2008},

date = {2008-01-01},

journal = {Zeitschrift fur Geomorphologie},

volume = {52},

number = {SUPPL. 2},

pages = {15-33},

abstract = {In Poland, first traces of human activity on dunes and areas of aeolian cover sands were observed in the Vistulian period. Man, however, was not an essential factor in the mobilisation of drift sands at the time because his main occupation was hunting and nemoriculture. At the beginning of the Holocene, the situation was not different. Intensive aeolian processes caused by human interference in the natural dune environments took place in the Sub-Boreal and Sub-Atlantic periods. It is assumed that they mainly consisted in the translocation of Late-Glacial dunes and the formation of thick and loose sandy series which were not of larger morphological significance (although Holocene dunes are also known). Aeolian series are frequently divided by fossil soils (mostly humus horizons) in which the occurrence of charcoal and pollen of synanthropic plants indicates pasturing and agricultural activity. Moreover, in dune sands, numerous artifacts belonging to different cultures have been found. The paper focuses on a synthesis of anthropogenically induced aeolian processes in the Silesian-Cracow Upland that has been the main area of investigation carried out by the Geographical Centre of the Silesian University in Sosnowiec, Poland. The research hypothesis is as follows: the Holocene aeolian processes in the Silesian-Cracow Upland are to a large extent related to activity of man, who used natural conditions of the region. The aim of this study is to analyse human-induced changes recorded in aeolian deposits and relief of this upland from a historical perspective against a background of the Holocene aeolian processes in Poland. To achieve this aim, we used numerous C14 datings, palynological analyses, archaeological finds (the reference to archaeological research being rather cursory), historical information, structural measurements and analyses of sand grain-size, analyses of archival and present cartographic materials, aerial photos and instrumental and non-instrumental observations of aeolian processes. Finally, periods of human interference recorded in aeolian deposits and relief have been distinguished. They are as follows: the Atlantic, the Sub-Boreal, the Sub-Atlantic, including the last millennium with a period of direct field observations, an analysis of changes and developmental tendencies of relief and determination of wind processes dynamics. © 2008 Gebrüder Borntraeger.},

note = {9},

keywords = {},

pubstate = {published},

tppubtype = {article}

}

In Poland, first traces of human activity on dunes and areas of aeolian cover sands were observed in the Vistulian period. Man, however, was not an essential factor in the mobilisation of drift sands at the time because his main occupation was hunting and nemoriculture. At the beginning of the Holocene, the situation was not different. Intensive aeolian processes caused by human interference in the natural dune environments took place in the Sub-Boreal and Sub-Atlantic periods. It is assumed that they mainly consisted in the translocation of Late-Glacial dunes and the formation of thick and loose sandy series which were not of larger morphological significance (although Holocene dunes are also known). Aeolian series are frequently divided by fossil soils (mostly humus horizons) in which the occurrence of charcoal and pollen of synanthropic plants indicates pasturing and agricultural activity. Moreover, in dune sands, numerous artifacts belonging to different cultures have been found. The paper focuses on a synthesis of anthropogenically induced aeolian processes in the Silesian-Cracow Upland that has been the main area of investigation carried out by the Geographical Centre of the Silesian University in Sosnowiec, Poland. The research hypothesis is as follows: the Holocene aeolian processes in the Silesian-Cracow Upland are to a large extent related to activity of man, who used natural conditions of the region. The aim of this study is to analyse human-induced changes recorded in aeolian deposits and relief of this upland from a historical perspective against a background of the Holocene aeolian processes in Poland. To achieve this aim, we used numerous C14 datings, palynological analyses, archaeological finds (the reference to archaeological research being rather cursory), historical information, structural measurements and analyses of sand grain-size, analyses of archival and present cartographic materials, aerial photos and instrumental and non-instrumental observations of aeolian processes. Finally, periods of human interference recorded in aeolian deposits and relief have been distinguished. They are as follows: the Atlantic, the Sub-Boreal, the Sub-Atlantic, including the last millennium with a period of direct field observations, an analysis of changes and developmental tendencies of relief and determination of wind processes dynamics. © 2008 Gebrüder Borntraeger.

Pełka-Gościniak, J.; Rahmonov, O.; Szczypek, T.

Water reservoirs in subsidence depressions in landscape of the Silesian Upland (Southern Poland) Proceedings

Vilnius Gediminas Technical University Publishing House "Technika", 2008, ISBN: 9789955282563, (4).

Abstract | Links | BibTeX