Bogumił Wicik
Datos Biográficos
| ID | 5599593 |
|---|---|
| NOMBRE | Bogumił Wicik |
| NOMBRES | Bogumił |
| APELLIDO | Wicik |
| FIRMA | WICIK B |
| AFILIACIONES | Geographical Faculty, Warsaw University, Warsaw, Poland |
| VERIFICADO | No |
| TOTAL DE OBRAS | 3 |
| TOTAL DE CITAS | 11 |
| TOTAL COMO AUTOR | 3 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1992 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 1996 |
| ÍNDICE H | 2 |
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…
Radiocarbon Chronology of Late Glacial and Holocene Sedimentation and Water-Level Changes in the Area of the Gościąż Lake Basin
We obtained 14 C ages on samples of lake marl and other sediments from cores taken in Gościąż Lake and its environs. Comparison of 14 C dates of bulk samples of laminated sediment with varve chronology and available AMS dates of terrestrial macrofossils indicates a reservoir correction of 2000 ± 120 yr for the basal series of lake sediments. 14 C dates obtained on peat layers underlying the oldest lacustrine sediments in Gościąż and other lakes c…
Possibilities for Reconstructing Radiocarbon Level Changes During the Late Glacial by Using a Laminated Sequence of Gościaż Lake
Laminated sediments of Gościaż Lake can be used as an independent source of material for calibrating the radiocarbon time scale. The varve chronology is based on three long cores from the deepest part of the lake, with one additional core from the second deepest part. From pollen and Cladocera spectra and stable isotope and chemical content sequences, we have determined the Allerød(AL)/Younger Dryas(YD) and Younger Dryas/Preboreal(PB) boundaries …
Possibilities for Reconstructing Radiocarbon Level Changes During the Late Glacial by Using a Laminated Sequence of Gościaż Lake
Laminated sediments of Gościaż Lake can be used as an independent source of material for calibrating the radiocarbon time scale. The varve chronology is based on three long cores from the deepest part of the lake, with one additional core from the second deepest part. From pollen and Cladocera spectra and stable isotope and chemical content sequences, we have determined the Allerød(AL)/Younger Dryas(YD) and Younger Dryas/Preboreal(PB) boundaries …
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…
Radiocarbon Chronology of Late Glacial and Holocene Sedimentation and Water-Level Changes in the Area of the Gościąż Lake Basin
We obtained 14 C ages on samples of lake marl and other sediments from cores taken in Gościąż Lake and its environs. Comparison of 14 C dates of bulk samples of laminated sediment with varve chronology and available AMS dates of terrestrial macrofossils indicates a reservoir correction of 2000 ± 120 yr for the basal series of lake sediments. 14 C dates obtained on peat layers underlying the oldest lacustrine sediments in Gościąż and other lakes c…
Possibilities for Reconstructing Radiocarbon Level Changes During the Late Glacial by Using a Laminated Sequence of Gościaż Lake
Laminated sediments of Gościaż Lake can be used as an independent source of material for calibrating the radiocarbon time scale. The varve chronology is based on three long cores from the deepest part of the lake, with one additional core from the second deepest part. From pollen and Cladocera spectra and stable isotope and chemical content sequences, we have determined the Allerød(AL)/Younger Dryas(YD) and Younger Dryas/Preboreal(PB) boundaries …
Radiocarbon Chronology of Late Glacial and Holocene Sedimentation and Water-Level Changes in the Area of the Gościąż Lake Basin
We obtained 14 C ages on samples of lake marl and other sediments from cores taken in Gościąż Lake and its environs. Comparison of 14 C dates of bulk samples of laminated sediment with varve chronology and available AMS dates of terrestrial macrofossils indicates a reservoir correction of 2000 ± 120 yr for the basal series of lake sediments. 14 C dates obtained on peat layers underlying the oldest lacustrine sediments in Gościąż and other lakes c…
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…
Geography (3 obras) · Geology (3 obras) · Geology and Paleoclimatology Research (3 obras) · Glacial period (3 obras) · Holocene (3 obras) · Paleontology (3 obras) · Physical geography (3 obras) · Sediment (3 obras) · Ancient and Medieval Archaeology Studies (2 obras) · Archaeology (2 obras)