Michał Gradziński
Datos Biográficos
| ID | 4640566 |
|---|---|
| NOMBRE | Michał Gradziński |
| NOMBRES | Michał |
| APELLIDO | Gradziński |
| FIRMA | GRADZIŃSKI M |
| AFILIACIONES | Jagiellonian University |
| ORCID | 0000-0001-7866-1376 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 6 |
| TOTAL DE CITAS | 5 |
| TOTAL COMO AUTOR | 6 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1999 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2025 |
| ÍNDICE H | 2 |
Growth rate of cave ice based on 14 C dating of fossil bats as a palaeoenvironmental proxy for the last 1300 years in the Western Carpathians
Among various palaeoclimatic analyses of the Late-Holocene, assessing the cave ice growth rate offers valuable insights into past environmental conditions. Dobšiná Ice Cave (DIC; Carpathians, Slovakia) is an impressive ice cave, which hosts one of the most extensive subterranean perennial ice block. Thirteen organic macroremains were collected from a clearly layered ice section ca. 12 m thick. 14 C dating of the samples enabled the construction o…
Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland
The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides importa…
Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)
Five stalagmites from the Demänová Cave System (DCS, Western Carpathians, Slovakia), spanning the period from 13,000 to 500 a BP, were analyzed for their oxygen and carbon stable isotopic composition of the calcite. The isotopic data obtained from several stalagmites located in one cave system allow us to separate the changes of regional/global importance from the local changes. Oxygen isotope ratios point to dynamic changes in the environment at…
Recently growing subaqueous flowstones
Sedimentation of Holocene tufa influenced by the Neolithic man
Variations of Isotopic Composition of Carbon in the Karst Environment from Southern Poland, Present and Past
We describe a comprehensive study of carbon isotopes in several karst springs and their environs in a contemporary karst environment in the region of the Cracow-Wieluñ Upland and Western Tatra Mountains, Southern Poland. We collected samples of water, plants and carbonate deposited on aquatic plants, and obtained 13 C values and 14 C concentrations. We also investigated a group of the youngest calcium carbonates from caves where deposition is sti…
Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland
The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides importa…
Variations of Isotopic Composition of Carbon in the Karst Environment from Southern Poland, Present and Past
We describe a comprehensive study of carbon isotopes in several karst springs and their environs in a contemporary karst environment in the region of the Cracow-Wieluñ Upland and Western Tatra Mountains, Southern Poland. We collected samples of water, plants and carbonate deposited on aquatic plants, and obtained 13 C values and 14 C concentrations. We also investigated a group of the youngest calcium carbonates from caves where deposition is sti…
Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)
Five stalagmites from the Demänová Cave System (DCS, Western Carpathians, Slovakia), spanning the period from 13,000 to 500 a BP, were analyzed for their oxygen and carbon stable isotopic composition of the calcite. The isotopic data obtained from several stalagmites located in one cave system allow us to separate the changes of regional/global importance from the local changes. Oxygen isotope ratios point to dynamic changes in the environment at…
Variations of Isotopic Composition of Carbon in the Karst Environment from Southern Poland, Present and Past
We describe a comprehensive study of carbon isotopes in several karst springs and their environs in a contemporary karst environment in the region of the Cracow-Wieluñ Upland and Western Tatra Mountains, Southern Poland. We collected samples of water, plants and carbonate deposited on aquatic plants, and obtained 13 C values and 14 C concentrations. We also investigated a group of the youngest calcium carbonates from caves where deposition is sti…
Recently growing subaqueous flowstones
Sedimentation of Holocene tufa influenced by the Neolithic man
Late Glacial and Holocene paleoecology and paleoenvironmental changes in the northern Carpathians foreland
The study of past environments, their ecology, and detailed changes through time has become an important task of environmental science. Records of paleoenvironment usually vary between regions owing to different influences of local climate, vegetation, relief, and depositional processes. Therefore, studying local sequences thoroughly allows paleoenvironmental and paleoecological reconstructions for particular regions, but it also provides importa…
Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)
Five stalagmites from the Demänová Cave System (DCS, Western Carpathians, Slovakia), spanning the period from 13,000 to 500 a BP, were analyzed for their oxygen and carbon stable isotopic composition of the calcite. The isotopic data obtained from several stalagmites located in one cave system allow us to separate the changes of regional/global importance from the local changes. Oxygen isotope ratios point to dynamic changes in the environment at…
Growth rate of cave ice based on 14 C dating of fossil bats as a palaeoenvironmental proxy for the last 1300 years in the Western Carpathians
Among various palaeoclimatic analyses of the Late-Holocene, assessing the cave ice growth rate offers valuable insights into past environmental conditions. Dobšiná Ice Cave (DIC; Carpathians, Slovakia) is an impressive ice cave, which hosts one of the most extensive subterranean perennial ice block. Thirteen organic macroremains were collected from a clearly layered ice section ca. 12 m thick. 14 C dating of the samples enabled the construction o…
Geology (6 obras) · Geology and Paleoclimatology Research (6 obras) · Archaeology (5 obras) · Cave (5 obras) · Paleontology (5 obras) · Geochemistry (4 obras) · Geography (4 obras) · Marine and environmental studies (4 obras) · Carbonate (3 obras) · Geomorphology (3 obras)