Leszek Starkel
Dados Biográficos
| ID | 3756844 |
|---|---|
| NOME | Leszek Starkel |
| PRENOMES | Leszek |
| SOBRENOME | Starkel |
| ASSINATURA | STARKEL L |
| AFILIAÇÕES | Polish Academy of Sciences |
| ORCID | 0000-0003-1365-441X |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 21 |
| TOTAL DE CITAÇÕES | 27 |
| TOTAL COMO AUTOR | 21 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1984 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2022 |
| ÍNDICE H | 3 |
Climatic Oscillations During Mis 3–2 Recorded in Sets of 14 C and Osl Dates—a Study Based on Data From Poland
Terrestrial environments tend to be characterized by an incomplete record of past conditions. For the MIS 3–2 periods, there is only one known site in Poland—Horoszki Duże—in which a probably continuous record of climate change has been preserved. However, this site does not have any high precision multi-proxy analyses. In the absence of continuous high-resolution records, we decided to gather and analyze scattered information. We assembled data …
Stratigraphy of alluvia and phases of the Holocene floods in the valleys of the Eastern Carpathians foreland
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
Fluvial history of the Sub-Carpathian Basins (Poland) during the last cold stage (60–8 cal ka BP)
Progress in the holocene chrono-climatostratigraphy of Polish territory
The Holocene delivers a unique possibility to establish climatic stratigraphic boundaries based on detailed chronostratigraphy reflected in various facies of continental sediments, in their lithological parameters and organic remains. These sediments are dated by the 14C method in the case of organic remains, by counting annual laminations in lacustrine facies, and by dendrochronological method in the case of fluvial sediments. The existence of w…
Medieval accumulation in the Upper Dniester river valley
Hydrological Changes After the Last Ice Retreat in Northern Poland Using Radiocarbon Dating
A simplified model of hydrological changes during the Late Glacial and Holocene is presented for the northern Polish regions that were ice covered during the Last Glacial. This reconstruction is based on a group of 197 radiocarbon dates from about 120 localities reflecting the sequence of alternating lake transgressions and regressions. The earliest transgressions were related to dead-ice melting (sometimes in 2–3 phases), while the later ones st…
Present-day events and the evaluation of Holocene palaeoclimatic proxy data
Past hydrological events reflected in the Holocene fluvial record of Europe
Change in the frequency of extreme events as the indicator of climatic change in the Holocene (in fluvial systems)
Global Continental Palaeohydrology
Lake-level and groundwater-level changes in the Lake Gosciąż area, Poland
Lake Gosciąz is located in the zone of the maximum extent of the last ice sheet. Distinct lake terraces and deposits related to the lateglacial transgression do not exist. Detailed examination of annually laminated sediments and landforms revealed three phases of higher water level and storage, represented by shore features, by littoral, deltaic and bog deposits, and by higher rates of lacustrine deposition in the pelagic zone. Holocene lake tran…
Reconstruction of hydrological changes between 7000 and 3000 BP in the upper and middle Vistula River Basin, Poland
Rhythmic fluctuations in the hydrological regime are demonstrated based on a review of records sensitive to relative climatic stability between 7000 and 3000 BP in the upper and middle parts of the Vistula River Basin, central Europe. In the fluvial deposits and landforms these variations are very clear; phases of higher flood frequency are dated 6600-6000, 5500-4750, 4500-4100 and 3250-3000 BP. These phases coincide very well with sparse informa…
Environmental changes at the Younger Dryas-Preboreal transition and during the early Holocene
Data on environmental change at the Younger Dryas-Preboreal transition and during the early Holocene are reviewed with particular reference to evidence from Poland and neighbouring areas of central Europe. Various factors modified the rate of environmental change during the general warming and reforestation. The preservation in central Europe of coniferous forest at the beginning of the Holocene, and the relatively late development of deciduous f…
Thresholds in the Transformation of Slopes and River Channels in the Darjeeling Himalaya, India
W. Froehlich, E. Gil, I. Kasza, L. Starkel, Thresholds in the Transformation of Slopes and River Channels in the Darjeeling Himalaya, India, Mountain Research and Development, Vol. 10, No. 4 (Nov., 1990), pp. 301-312
Global paleohydrology
Stable Isotopes of Holocene Calcareous Tufa in Southern Poland as Paleoclimatic Indicators
The isotopic composition of oxygen in freshwater calcareous tufa seems to be a sensitive indicator of past climatic changes. Results of measurements of δ c 18 O and δ c 13 C in tufa samples dated with the 14 C method are used to reconstruct Holocene climatic changes in southern Poland. Values of δ c 18 O obtained on tufa samples from four sites (Raclawka, Rzerzuŝnia, Trzebienice, Sieradowice) representing different hydrodynamic conditions of tufa…
British Geomorphological Research Group
The 1
Changes of the Vistula River channel and floodplain in the last 200 years
Evolution of the Vistula River Valley during the last 15000 years
Environmental changes at the Younger Dryas-Preboreal transition and during the early Holocene
Data on environmental change at the Younger Dryas-Preboreal transition and during the early Holocene are reviewed with particular reference to evidence from Poland and neighbouring areas of central Europe. Various factors modified the rate of environmental change during the general warming and reforestation. The preservation in central Europe of coniferous forest at the beginning of the Holocene, and the relatively late development of deciduous f…
Global Continental Palaeohydrology
Lake-level and groundwater-level changes in the Lake Gosciąż area, Poland
Lake Gosciąz is located in the zone of the maximum extent of the last ice sheet. Distinct lake terraces and deposits related to the lateglacial transgression do not exist. Detailed examination of annually laminated sediments and landforms revealed three phases of higher water level and storage, represented by shore features, by littoral, deltaic and bog deposits, and by higher rates of lacustrine deposition in the pelagic zone. Holocene lake tran…
Reconstruction of hydrological changes between 7000 and 3000 BP in the upper and middle Vistula River Basin, Poland
Rhythmic fluctuations in the hydrological regime are demonstrated based on a review of records sensitive to relative climatic stability between 7000 and 3000 BP in the upper and middle parts of the Vistula River Basin, central Europe. In the fluvial deposits and landforms these variations are very clear; phases of higher flood frequency are dated 6600-6000, 5500-4750, 4500-4100 and 3250-3000 BP. These phases coincide very well with sparse informa…
Climatic Oscillations During Mis 3–2 Recorded in Sets of 14 C and Osl Dates—a Study Based on Data From Poland
Terrestrial environments tend to be characterized by an incomplete record of past conditions. For the MIS 3–2 periods, there is only one known site in Poland—Horoszki Duże—in which a probably continuous record of climate change has been preserved. However, this site does not have any high precision multi-proxy analyses. In the absence of continuous high-resolution records, we decided to gather and analyze scattered information. We assembled data …
British Geomorphological Research Group
The 1
Stable Isotopes of Holocene Calcareous Tufa in Southern Poland as Paleoclimatic Indicators
The isotopic composition of oxygen in freshwater calcareous tufa seems to be a sensitive indicator of past climatic changes. Results of measurements of δ c 18 O and δ c 13 C in tufa samples dated with the 14 C method are used to reconstruct Holocene climatic changes in southern Poland. Values of δ c 18 O obtained on tufa samples from four sites (Raclawka, Rzerzuŝnia, Trzebienice, Sieradowice) representing different hydrodynamic conditions of tufa…
Global paleohydrology
Thresholds in the Transformation of Slopes and River Channels in the Darjeeling Himalaya, India
W. Froehlich, E. Gil, I. Kasza, L. Starkel, Thresholds in the Transformation of Slopes and River Channels in the Darjeeling Himalaya, India, Mountain Research and Development, Vol. 10, No. 4 (Nov., 1990), pp. 301-312
Environmental changes at the Younger Dryas-Preboreal transition and during the early Holocene
Data on environmental change at the Younger Dryas-Preboreal transition and during the early Holocene are reviewed with particular reference to evidence from Poland and neighbouring areas of central Europe. Various factors modified the rate of environmental change during the general warming and reforestation. The preservation in central Europe of coniferous forest at the beginning of the Holocene, and the relatively late development of deciduous f…
Reconstruction of hydrological changes between 7000 and 3000 BP in the upper and middle Vistula River Basin, Poland
Rhythmic fluctuations in the hydrological regime are demonstrated based on a review of records sensitive to relative climatic stability between 7000 and 3000 BP in the upper and middle parts of the Vistula River Basin, central Europe. In the fluvial deposits and landforms these variations are very clear; phases of higher flood frequency are dated 6600-6000, 5500-4750, 4500-4100 and 3250-3000 BP. These phases coincide very well with sparse informa…
Lake-level and groundwater-level changes in the Lake Gosciąż area, Poland
Lake Gosciąz is located in the zone of the maximum extent of the last ice sheet. Distinct lake terraces and deposits related to the lateglacial transgression do not exist. Detailed examination of annually laminated sediments and landforms revealed three phases of higher water level and storage, represented by shore features, by littoral, deltaic and bog deposits, and by higher rates of lacustrine deposition in the pelagic zone. Holocene lake tran…
Global Continental Palaeohydrology
Change in the frequency of extreme events as the indicator of climatic change in the Holocene (in fluvial systems)
Past hydrological events reflected in the Holocene fluvial record of Europe
Present-day events and the evaluation of Holocene palaeoclimatic proxy data
Progress in the holocene chrono-climatostratigraphy of Polish territory
The Holocene delivers a unique possibility to establish climatic stratigraphic boundaries based on detailed chronostratigraphy reflected in various facies of continental sediments, in their lithological parameters and organic remains. These sediments are dated by the 14C method in the case of organic remains, by counting annual laminations in lacustrine facies, and by dendrochronological method in the case of fluvial sediments. The existence of w…
Medieval accumulation in the Upper Dniester river valley
Hydrological Changes After the Last Ice Retreat in Northern Poland Using Radiocarbon Dating
A simplified model of hydrological changes during the Late Glacial and Holocene is presented for the northern Polish regions that were ice covered during the Last Glacial. This reconstruction is based on a group of 197 radiocarbon dates from about 120 localities reflecting the sequence of alternating lake transgressions and regressions. The earliest transgressions were related to dead-ice melting (sometimes in 2–3 phases), while the later ones st…
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
Fluvial history of the Sub-Carpathian Basins (Poland) during the last cold stage (60–8 cal ka BP)
Stratigraphy of alluvia and phases of the Holocene floods in the valleys of the Eastern Carpathians foreland
Climatic Oscillations During Mis 3–2 Recorded in Sets of 14 C and Osl Dates—a Study Based on Data From Poland
Terrestrial environments tend to be characterized by an incomplete record of past conditions. For the MIS 3–2 periods, there is only one known site in Poland—Horoszki Duże—in which a probably continuous record of climate change has been preserved. However, this site does not have any high precision multi-proxy analyses. In the absence of continuous high-resolution records, we decided to gather and analyze scattered information. We assembled data …
Changes of the Vistula River channel and floodplain in the last 200 years
Evolution of the Vistula River Valley during the last 15000 years
Geography (19 obras) · Geology (16 obras) · Geology and Paleoclimatology Research (16 obras) · Physical geography (16 obras) · Holocene (11 obras) · Paleontology (10 obras) · Archaeology (8 obras) · Geology (8 obras) · Geomorphology (8 obras) · Climatology (7 obras)