Jarosław Sikorski
Biographic Data
| ID | 6572246 |
|---|---|
| NAME | Jarosław Sikorski |
| GIVEN NAMES | Jarosław |
| FAMILY NAME | Sikorski |
| SIGNATURE | SIKORSKI J |
| AFFILIATIONS | Silesian University of Technology |
| ORCID | 0000-0001-5363-8866 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 11 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2009 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 1 |
Intense and quick land relief transformation in the Little Ice Age
Carbon accumulation rates in two poor fens with different water regimes
Fens are underestimated carbon sinks. Knowledge about their role in the sequestration of CO 2 in the past is limited. The research reported here focused on identifying long-term carbon accumulation rates (CARs) in a drained fen (Bagno Bruch) and a waterlogged fen (Bagno Mikołeska) in southern Poland. On the basis of 210 Pb and AMS 14 C dates and age–depth modeling, 7000- and 2000-year records of changes in bulk composition and carbon and sulfur c…
Multiproxy evidence of `Little Ice Age' palaeoenvironmental changes in a peat bog from northern Poland
`Little Ice Age' (LIA) climatic deteriorations have been abundantly documented in various archives such as ice, lake sediments and peat bog deposits. Palaeoecological analyses of peat samples have identified these climatic deteriorations using a range of techniques, for example palynology, plant macrofossils, testate amoebae or carbon isotopic analyses. The use of inorganic geochemistry and the reconstruction of dust fluxes has remained a challen…
Multiproxy evidence of `Little Ice Age' palaeoenvironmental changes in a peat bog from northern Poland
`Little Ice Age' (LIA) climatic deteriorations have been abundantly documented in various archives such as ice, lake sediments and peat bog deposits. Palaeoecological analyses of peat samples have identified these climatic deteriorations using a range of techniques, for example palynology, plant macrofossils, testate amoebae or carbon isotopic analyses. The use of inorganic geochemistry and the reconstruction of dust fluxes has remained a challen…
Multiproxy evidence of `Little Ice Age' palaeoenvironmental changes in a peat bog from northern Poland
`Little Ice Age' (LIA) climatic deteriorations have been abundantly documented in various archives such as ice, lake sediments and peat bog deposits. Palaeoecological analyses of peat samples have identified these climatic deteriorations using a range of techniques, for example palynology, plant macrofossils, testate amoebae or carbon isotopic analyses. The use of inorganic geochemistry and the reconstruction of dust fluxes has remained a challen…
Carbon accumulation rates in two poor fens with different water regimes
Fens are underestimated carbon sinks. Knowledge about their role in the sequestration of CO 2 in the past is limited. The research reported here focused on identifying long-term carbon accumulation rates (CARs) in a drained fen (Bagno Bruch) and a waterlogged fen (Bagno Mikołeska) in southern Poland. On the basis of 210 Pb and AMS 14 C dates and age–depth modeling, 7000- and 2000-year records of changes in bulk composition and carbon and sulfur c…
Intense and quick land relief transformation in the Little Ice Age
Archaeology (3 works) · Geography (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Physical geography (3 works) · Climate change (2 works) · Deposition (geology (2 works) · Environmental Science (2 works) · Holocene (2 works) · Oceanography (2 works)