Andriy K Cheburkin
Biographic Data
| ID | 6572265 |
|---|---|
| NAME | Andriy K Cheburkin |
| GIVEN NAMES | Andriy K |
| FAMILY NAME | Cheburkin |
| SIGNATURE | CHEBURKIN A K |
| AFFILIATIONS | Heidelberg University |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 12 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1998 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 1 |
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…
Six millennia of atmospheric dust deposition in southern South America (Isla Navarino, Chile)
To characterize dust deposition in southern South America for the Holocene, a 542 cm long core from a peat bog in southern Chile (Oreste bog, Isla Navarino) was studied. Peat formation started ~11 160 14 C yr before present (BP). The titanium (Ti) concentration in bulk peat, combined with dry bulk density, and peat accumulation rate, were used to calculate the mineral accumulation rate (MAR) in the Oreste bog. The distribution of calcium (Ca), ma…
History of Atmospheric Lead Deposition Since 12,370 14 C yr BP from a Peat Bog, Jura Mountains, Switzerland
A continuous record of atmospheric lead since 12,370 carbon-14 years before the present ( 14 C yr BP) is preserved in a Swiss peat bog. Enhanced fluxes caused by climate changes reached their maxima 10,590 14 C yr BP (Younger Dryas) and 8230 14 C yr BP. Soil erosion caused by forest clearing and agricultural tillage increased lead deposition after 5320 14 C yr BP. Increasing lead/scandium and decreasing lead-206/lead-207 beginning 3000 14 C yr BP…
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…
Six millennia of atmospheric dust deposition in southern South America (Isla Navarino, Chile)
To characterize dust deposition in southern South America for the Holocene, a 542 cm long core from a peat bog in southern Chile (Oreste bog, Isla Navarino) was studied. Peat formation started ~11 160 14 C yr before present (BP). The titanium (Ti) concentration in bulk peat, combined with dry bulk density, and peat accumulation rate, were used to calculate the mineral accumulation rate (MAR) in the Oreste bog. The distribution of calcium (Ca), ma…
History of Atmospheric Lead Deposition Since 12,370 14 C yr BP from a Peat Bog, Jura Mountains, Switzerland
A continuous record of atmospheric lead since 12,370 carbon-14 years before the present ( 14 C yr BP) is preserved in a Swiss peat bog. Enhanced fluxes caused by climate changes reached their maxima 10,590 14 C yr BP (Younger Dryas) and 8230 14 C yr BP. Soil erosion caused by forest clearing and agricultural tillage increased lead deposition after 5320 14 C yr BP. Increasing lead/scandium and decreasing lead-206/lead-207 beginning 3000 14 C yr BP…
Six millennia of atmospheric dust deposition in southern South America (Isla Navarino, Chile)
To characterize dust deposition in southern South America for the Holocene, a 542 cm long core from a peat bog in southern Chile (Oreste bog, Isla Navarino) was studied. Peat formation started ~11 160 14 C yr before present (BP). The titanium (Ti) concentration in bulk peat, combined with dry bulk density, and peat accumulation rate, were used to calculate the mineral accumulation rate (MAR) in the Oreste bog. The distribution of calcium (Ca), ma…
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…
Archaeology (3 works) · Bog (3 works) · Geography (3 works) · Geology and Paleoclimatology Research (3 works) · Peat (3 works) · Chemistry (2 works) · Deposition (geology (2 works) · Environmental Science (2 works) · Geology (2 works) · Geomorphology (2 works)