Autor: Moska, Piotr - Prolib Integro

Skocz do pozycji: 1.

Tytuł:: Luminescence dating of Quaternary sediments – some practical aspects
Autorzy:: Moska, Piotr
Tematy:: luminescence dating
dose rate
equivalent dose; Pokaż więcej
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Powiązania:: https://bibliotekanauki.pl/articles/2025218.pdf Link otwiera się w nowym oknie
Opis:: Luminescence dating is based mainly on the dosimetric properties of quartz and feldspar. These minerals are among the most popular found on Earth, resulting in the possibility of using luminescence methods in practically any environment. Currently, quartz remains the best recognized mineral in terms of dosimetric properties, particularly with regards to results obtained for quartz grains, which are regarded as being the most reliable in luminescence dating. Supporters of luminescence methods are constantly growing, however, these groups do not always have sufficient knowledge to avoid even the most basic of issues that may be encountered overall – from the process of sampling through to the awareness of what a single luminescence result represents. The present paper provides an overview of several practical aspects of luminescence dating such as correct sampling procedures and all necessary information regarding the calculation of the dose rate and equivalent dose with particular reference to potential problems that occur when the age of the sample is being determined. All these aspects are crucial for obtaining a reliable dating result, on the other hand, they remain a potential source of uncertainty.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: New perspectives of dating prehistoric soil erosion in loess areas = Nowe perspektywy datowania pradziejowej erozji gleb w obszarach lessowych
Sprawozdania Archeologiczne 64 (2012)
Autorzy:: Poręba, Grzegorz J.
Moska, Piotr
Śnieszko, Zbigniew
Wydawca:: Instytut Archeologii i Etnologii Polskiej Akademii Nauk
Powiązania:: Kruk J. 1980. Gospodarka w Polsce południowo-wschodniej w V–III tysiącleciu p.n.e. Ossolineum. Wrocław: Ossolineum
Galbraith R. F., Roberts R. G., Laslett G. M.,Yoshida H. and Olley J. M. 1999. Optical dating of single and multiple grains of quatz from Iinmimum rock shelter, Northen Australia; part 1, eksperimental design and statistical models. Archaeometry 41, 339–364
Kaiser K., Schoh W. H. and Miehe G. 2007. Holocene paleosols and colluvial sediments in Northeast Tibet (Qinghai Province, China): Properties, dating and paleoenvironmental implications. Catena 69, 91–102
Kruk J. 2008. Wzory przeszłości . Studia nad neolitem środkowym i późnym. Kraków: Instytut Archeologiii Etnologii Polskiej Akademii Nauk
Kruk J., Milisauskas S., Alexandrowicz S. W. and Śnieszko Z. 1996. Osadnictwo i zmiany środowiska naturalnego wyżyn lessowych. Kraków: Instytut Archeologii i Etnologii PAN
Bluszcz A., Poręba G. J. and Śnieszko Z. 2007. The basis of the study of the age of the Holocene deluvium on loess areas of Polish highlands. Geochronometria 28, 61–66
Kruk J. 1993. Rozwój społeczno-gospodarczy i zmiany środowiska przyrodniczego wyżyn lessowych w neolicie (4800–1800 bc). Sprawozdania Archeologiczne 45, 7–17
Kruk J. and Milisauskas S. 1999. Rozkwit i upadek społeczeństw rolniczych neolitu. Kraków: Instytut Archeologii i Etnologii Polskiej Akademii Nauk
Maruszczak H. 1988. Zmiany środowiska przyrodniczego kraju w czasach historycznych. In L. Starkel (Ed.), Przemiany środowiska geograficznego Polski. Wrocław: Ossolineum, 109–137
Sprawozdania Archeologiczne
Lu Y.C., Wang X.L. and Wintle A. G. 2007. A new OSL chronology for dust accumulation in the last 130,000 yr. for the Chinese Loess Plateau. Quaternary Research 67(1), 152–160
Maruszczak H. 1973. Erozja wąwozowa we wschodniej części pasa wyżyn południowopolskich. Zeszyty Problem. Post. Nauk Roln. 151, 30
Buckman- Nyle H. C. and Brady C. 1969. The Nature and Properties of Soils. Seventh Edition. New York: Macmillan [Polish ed. Buckman- Nyle H. C., Brady C. 1971. Gleba i jej właściwości. Warszawa: PWRi L]
Kruk J. 1973. Studia osadnicze nad neolitem wyżyn lessowych. Wrocław: Ossolineum
Śnieszko Z. 1995, Ewolucja obszarów lessowych Wyżyn Polskich w czasie ostatnich 15 000 lat. Katowice: Wydawnictwo Uniwersytetu Śląskiego
Poręba G., Śnieszko Z. and Moska P. 2011. Some aspects of age assessment of Holocene less colluvium; OSL and 137Cs dating of sediment from Biała agricultural area, South Poland. Quaternary International 240(1–2). 44–51
Maruszczak H. and Trębaczowski J. 1956. Geomorfologiczne skutki gwałtownej ulewy w Piaskach Szlacheckich koło Krasnegostawu. Annales UMCS, Sec. B 11(4), 129–151
Dwucet K. and Śnieszko Z. 1997 . Zmiany fizykochemiczne cech lessów i gleb nalessowych po redepozycji spowodowanej gwałtowna ulewą. In L. Starkel (ed.), Rola gwałtownych ulew w ewolucji rzeźby Wyżyny Miechowskiej (na przykładzie ulewy w dniu 15 września 1995 roku). (= Dokumentacja Geograficzna 8). Wrocław: IGIPZ PAN, 76–86
Poręba G. 2006. Zastosowanie 137 Cs do modelowania procesów erozji i akumulacji na obszarach lessowych. Gliwice
Śnieszko Z. 1985. Paleogeografia holocenu w dolinie Sancygniówki (= Acta Geographica Lodziensia 51). Łódź: ŁTN
Poręba G. J., Śnieszko Z. and Moska P. In Press. Influence of pedon history and washing nature on luminescence dating of Holocene colluvium on the example of research on the Polish loess areas. Quaternary International. Starkel L. (ed.) 1997. Rola gwałtownych ulew w ewolucji rzeźby Wyżyny Miechowskiej (na przykładzie ulewy w dniu 15 września 1995 roku) (= Dokumentacja Geograficzna 8). Wrocław: IGIPZ PAN
Klimaszewski M. 1978. Geomorfologia. Warszawa: PWN
Lai Z. P. 2010. Chronology and the upper dating limit for loess samples from Luochuan section in the Chinese Loess Plateau using quartz OSL SAR protocol. Journal of Asian Earth Sciences 37 2, 176–185
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Klimek K. 2003. Sediment transfer and storage linked to Neolithic and Early Medieval soil erosion In the Upper Odra Basin, southern Poland. In A. J. Howard, M. G . Macklin and D. G. Passmore (eds.), Alluvial Archeology in Europe. Lisse: Swets&Zeitlinger, 251–259
Opis:: This study presents the results of Optically Stimulated Luminescence (OSL) dating of colluvial sedimentprofiles from Biedrzykowice and Świerklany in the archaeologically well documented loess area of southernPoland, The method, the criteria for site selection and the limitations of the interpretation of the dates obtainedare discussed. It is shown that Holocene colluvial sediments containing grains of quartz can be approximatelydated using OSL. Despite its many limitations, it remains the only method suitable for direct dating of colluvialsediments. The obtained OSL dates are consistent with the archaeological evidence. The Biedrzykowice profile,located 6 km from the Neolithic settlement at Bronocice, contains two layers of Holocene colluvial sediments.The older layer, OSL dated to 6–5 ka BP, is separated from the younger, medieval layer dated to 1,0–0,5 ka BPby a fossil soil. In Świerklany, where there are no known prehistoric settlements, the accumulation of colluvialsediments only started in the medieval period. The OSL dating confirms earlier assumptions that in naturalHolocene ecosystems in loess areas of the moderate climate forest zones, mineral material was not transportedby slope wash, or only to a minimal extent. This work is the first direct isotopic dating of colluvial sediments inPoland
il. ; 25 cm
ill. ; 25 cm
Dostawca treści:: RCIN - Repozytorium Cyfrowe Instytutów Naukowych

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Skocz do pozycji: 3.

Tytuł:: Stratygraficzne i przestrzenne aspekty zróżnicowania składu chemicznego późnoplejstoceńskich sekwencji lessowo-glebowych w Polsce – przykłady profili w Tyszowcach i Białym Kościele
The stratigraphic and spatial aspects of the differentiation of the chemical composition of the Late Pleistocene loess-palaeosol sequences in Poland – a case study of the Tyszowce and Biały Kościół profiles
Autorzy:: Skurzyński, Jacek
Jary, Zdzisław
Raczyk, Jerzy
Moska, Piotr
Krawczyk, Marcin
Tematy:: less,
gleba kopalna
geochemia
wskaźniki wietrzeniowe
metoda chemostratygraficzna
loess
palaeosol
geochemistry
weathering indices
chemostratigraphic method; Pokaż więcej
Wydawca:: Łódzkie Towarzystwo Naukowe
Powiązania:: https://bibliotekanauki.pl/articles/578343.pdf Link otwiera się w nowym oknie
Opis:: Artykuł prezentuje porównanie składu geochemicznego i stopnia zwietrzenia chemicznego dwóch późnoplejstoceńskich sekwencji lessowo-glebowych, zlokalizowanych w SE i SW Polsce. Analiza chemiczna w zakresie pierwiastków głównych (Si, Al, Fe, Mn, Mg, Ca, Na, K, Ti, P) oraz wyliczonych na ich podstawie wskaźników (CIA, Ti/Al, K/Al, Mg/Ca, K/Ca, Na/K oraz Si/Al) wykazała, że obie sekwencje są zróżnicowane zarówno w ujęciu stratygraficznym, jak i przestrzennym. Zmienność stratygraficzna związana jest ze zmianami paleoklimatu warunkującymi natężenie zarówno procesów lito-, jak i pedogenezy. Zmienność przestrzenna może wynikać m.in. z odmiennych warunków klimatycznych w trakcie tworzenia się sekwencji lessowo-glebowych, recyklingu lessów lub nawet odmiennego źródła materiału. Istotna może być też dysproporcja miąższości sekwencji, skutkująca zróżnicowanym wpływem infiltracji wód opadowych.
The article presents the comparison of the geochemical composition and the degree of chemical weathering between two Late Pleistocene loess-palaeosol sequences of SE and SW Poland. The results of major element (Si, Al, Fe, Mn, Mg, Ca, Na, K, Ti, P) and geochemical index (CIA, Ti/Al, K/Al, Mg/Ca, K/Ca, Na/K oraz Si/Al) analyses indicate stratigraphical and spatial differentiation between sequences. The stratigraphic differentiation is connected with palaeoclimatic conditions which control the intensity of pedogenesis. The spatial variability may be attributed to different climatic conditions during the deposition of loess, the loess recycling process, or even to different source areas. The disproportion between the thicknesses of the loess covers can also be important. It can affect the rainwater infiltration effect.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Chronology of the Szeletian settlement at the site Lubotyń 11, Głubczyce district, in the light of Bayesian age modelling
Chronologia osadnictwa szeleckiego na stanowisku Lubotyń 11, pow. głubczycki, w świetle bayesowskiego modelowania datowań
Autorzy:: Jary, Zdzisław
Raczyk, Jerzy
Bobak, Dariusz
Moska, Piotr
Połtowicz-Bobak, Marta
Wydawca:: Muzeum Okręgowe w Rzeszowie
Cytata wydawnicza:: Bobak, D., Połtowicz-Bobak, M., Jary, Z., Raczyk, J., Moska, P., 2016. Chronologia osadnictwa szeleckiego na stanowisku Lubotyń 11, pow. głubczycki, w świetle bayesowskiego modelowania datowań. Materiały i Sprawozdania Rzeszowskiego Ośrodka Archeologicznego 37, 7–16. doi:10.15584/misroa.2016.37.1
Opis:: This article attempts to clarify the Szeletian chronology of the site Lubotyń 11 on the Głubczyce Plateau. The site, maintained in a good condition, has a series of radiocarbon and OSL dating. By the use of the method of Bayesian modelling, a model has been constructed, taking into account the stratigraphic relationships between the natural and cultural events observed at the site. It allowed us to restore the history of the site and, in particular, to establish two facts regarding the Palaeolithic settlement. Although the site is a remnant of multiple stays of human groups, and the flint material clearly indicates the presence of older and younger Szeletian phase, now it is not possible to separate chronologically settlement episodes. The established beginning of the settlement appears to be the earliest known chronological point within the operation of the Szeletian culture.
Dostawca treści:: Repozytorium Centrum Otwartej Nauki

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Skocz do pozycji: 5.

Tytuł:: Fluvial response to environmental changes during MIS 4-3: a sedimentary record at the Brześnica site, central-western Poland
Autorzy:: Moskalewicz, Damian
Tylmann, Karol
Woźniak, Piotr Paweł
Kopyść, Natalia
Moska, Piotr
Tematy:: braided river
fluvial deposits
OSL dating
MIS 4
MIS 3
Last Glacial Maximum; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2060131.pdf Link otwiera się w nowym oknie
Opis:: Fluvial deposits subjected to this study are exposed at the Brześnica site, in the south-western part of the Wielkopolska region in Poland, which was close to the ice-sheet limit during the Last Glacial Maximum (LGM). Sedimentological analyses, including lithofacies descriptions, palaeocurrent measurements, grain size and rounding analyses and heavy mineral compositions indicate that the fluvial deposits at Brześnica were deposited in braided river environment. The following fluvial sedimentary processes were inferred: (1) shallow, rapid flow alternating with waning flow, (2) infilling of erosional channels with fluvial sediments during flood events, (3) changes from supercritical to subcritical flows, and (4) shallow sheet floods. The results of OSL dating indicated sediment deposition ~65.2 ±1.5 ka, i.e. in MIS 4, that was here characterized by cold environmental conditions and a general shift from meandering to braided fluvial sedimentation style. This finding contrasts with accumulation/erosion phases interpreted previously in this region for that time interval; however, it is consistent with recent studies of fluvial systems functioning during MIS 5-2 and of factors responsible for sedimentation style.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: Erosion and accumulation phases during the last glacial-interglacial cycle : a case study of the terrace system of the Odra and Osobłoga rivers (southern Poland)
Autorzy:: Wójcicki, Krzysztof Jan
Pawelec, Halina
Malik, Ireneusz
Woskowicz-Ślęzak, Beata
Moska, Piotr
Tematy:: fluvial processes
river terraces
Late Quaternary
OSL
southern Poland; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2058537.pdf Link otwiera się w nowym oknie
Opis:: In the Odra and Osobłoga River valleys in the vicinity of the town of Krapkowice, a system of morphological levels is present which is exceptionally extensive compared to other such systems in southern Poland. The extent, origins and chronology of these levels have been the subject of many controversies. In the light of current research, the terraces, which are situated on average 14.5-13, 12-10, 8-6, 6-4 and 3-1 metres above the river level, were formed in the post-Wartanian interval. The main factor driving their development was erosion, which compensated for the effects of large-scale aggradation that had occurred during the anaglacial phase of the Odranian Glaciation (MIS 8) dated to 261 ±15 ka. The impact of climatic conditions on the trends towards fluvial erosion or accumulation was only of secondary importance. According to OSL dating, successive phases of vertical stabilisation of the valley floor occurred ~118.8 ±8.3, 87.7 ±5.7 and 42.0 ±2.0 ka. In the meantime, erosion intensified, which resulted in the formation of lower terrace levels. During the climatic minimum of the Upper Plenivistulian (21.5 ±1.5 ka), under conditions of the delivery of sheet-wash-generated sediment, the aggradation of distal reaches of the Odra River valley was locally marked. During the Late Vistulian and Holocene, erosive tendencies continued, which were reflected by the fact that the surfaces of subsequent inset alluvial fills were situated ever lower. In the light of dating results, it can be concluded that during the colder periods correlated with the Rederstall Stadial (MIS 5b) and with the Hasselo Stadial (MIS 3), a braided river was present in the river valleys examined, which was most probably accompanied by permafrost. During the Eemian Interglacial (MIS 5e), during the Late Vistulian Interstadials and in the Holocene, it was a meandering river.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 7.

Tytuł:: Late Middle Palaeolithic and Early Upper Palaeolithic in Poland in the light of new numerical dating
Geographia Polonica Vol. 97 No. 3 (2024)
Autorzy:: Moska, Piotr. Autor
Wiśniewski, Andrzej. Autor
Połtowicz-Bobak, Marta. Autor
Bobak, Dariusz. Autor
Wydawca:: IGiPZ PAN
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Opis:: Although the first numerical dating of Middle and Upper Palaeolithic sites in Poland was applied at the beginning of the second half of the 20th century, it has only been in the last two decades that a data increase has been recorded, making it possible to discuss both the development of human behaviour and cultural phenomena in time perspective. This paper aims to show the chronological diversity of sites dating from the beginning of the Weichselian glaciation (MIS 5a – MIS 5d, GI-19 – GI-23, Greenland Interstadials) to the middle part of MIS 3 (GI-8 – GI-10). We considered sites dated mainly by thermoluminescence dating (OSL) and radiocarbon dating. We relied on a series of recent datings. We attempted to analyse the stratigraphic integrity, the archaeological finds and the numerical dating results. Through OSL dating, we could establish the chronology of Micoquian sites, previously regarded as middle Pleistocene, to the last glaciation. The dating compilation also shows that the Late Middle Palaeolithic and Early Upper Palaeolithic (EUP) sites are unlikely to overlap, or if they do, it is only over a small period. Unfortunately, this period is poorly interpreted because it spans the limit of the radiocarbon dating reliability and goes beyond the bounds of the calibration curve. Confronting the datings of the Lincombian-Ranisian-Jerzmanowician (LRJ) complex and the oldest finds associated with Aurigniacian sites in Poland lead to the conclusion that these sites may have co-occurred for some time.
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Tytuł:: Chronology of the last ice sheet decay on the southern Baltic area based on dating of glaciofluvial and ice-dammed lake deposits
Autorzy:: Uścinowicz, Szymon
Adamiec, Grzegorz
Bluszcz, Andrzej
Jegliński, Wojciech
Jurys, Leszek
Miotk-Szpiganowicz, Grażyna
Moska, Piotr
Pączek, Urszula
Piotrowska, Natalia
Poręba, Grzegorz
Przezdziecki, Piotr
Uścinowicz, Grzegorz
Tematy:: southern Baltic area
deglaciation
Late Glacial
Słupsk Bank Phase
OSL dating; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2058614.pdf Link otwiera się w nowym oknie
Opis:: The paper presents the results of the first OSL dating of glaciofluvial and ice-marginal lake sediments which occur between end moraines of the Słupsk Bank and the Polish coast. The sand and gravel of glaciofluvial deltas on the Słupsk Bank were deposited most likely during a period from 14.3 ±1.2 to 16.6 ±1.4 ka ago. The deposition of silty-sandy sediments of the ice-marginal lake is dated at 14.51 ±0.81 and 14.6 ±1.4 ka years. Likewise, dates ranging from 13.74 ±0.84 to 16.70 ±1.1 ka obtained from low sandy ridges, related to the southern range of the ice-marginal lake in the Gardno-Łeba Lowland, indicate the most likely timing of their deposition. It can be concluded that a short stop of the ice sheet on the Słupsk Bank took place approximately 15.2 ka ago, which could be correlated with the position of the ice sheet front in central Skåne and in northern Lithuania at that time. Older and younger results were also obtained, except the dates mentioned above. The older ages show little sunlight exposure of sediments during their deposition. The younger dates indicate a marine origin of the sediments and show that some parts of glaciofluvial sediments were redeposited and exposed to sunlight at a later stage, most probably when dead-ice blocks were melting.
Dostawca treści:: Biblioteka Nauki

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