Irina Panyushkina
Biographic Data
| ID | 5597640 |
|---|---|
| NAME | Irina Panyushkina |
| GIVEN NAMES | Irina |
| FAMILY NAME | Panyushkina |
| SIGNATURE | PANYUSHKINA I |
| AFFILIATIONS | Tucson, USA |
| VERIFIED | No |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 22 |
| WORKS AS AUTHOR | 9 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2007 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 2 |
In Memoriam Stepan G. Shiyatov 1933–2021
Ancient human genomes from across the Eurasian steppes
More Rapid 14 C Excursions in the Tree-Ring Record
Two radiocarbon ( 14 C) excursions are caused by an increase of incoming cosmic rays on a short time scale found in the Late Holocene (AD 774–775 and AD 993–994), which are widely explained as due to extreme solar proton events (SPE). In addition, a larger event has also been reported at 5480 BC (Miyake et al. 2017a), which is attributed to a special mode of a grand solar minimum, as well as another at 660 BC (Park et al. 2017). Clearly, other ev…
Deglacial Hydroclimate of Midcontinental North America
During the last deglaciation temperatures over midcontinental North America warmed dramatically through the Bølling-Allerød, underwent a cool period associated with the Younger-Dryas and then reverted to warmer, near modern temperatures during the early Holocene. However, paleo proxy records of the hydroclimate of this period have presented divergent evidence. We reconstruct summer relative humidity (RH) across the last deglacial period using a m…
Radiocarbon and Tree-Ring Dates of the Bes-Shatyr #3 Saka Kurgan in the Semirechiye, Kazakhstan
This study employs tree-ring crossdating and radiocarbon measurements to determine the precise calendar age of the Bes-Shatyr Saka necropolis (43°47′N, 81°21′E) built for wealthy tribe leaders in the Ili River Valley (Semirechiye), southern Kazakhstan. We developed a 218-yr tree-ring chronology and a highly resolved sequence of 14 C from timbers of Bes-Shatyr kurgan #3. A 4-decadal-point 14 C wiggle dates the Bes-Shatyr necropolis to 600 cal BC. …
Impacts of cooling climate on prehistoric herding and farming strategies during the Bronze-Iron Age transition on the margins of the Eurasian steppe
High-resolution terrestrial MIS3 environment from trees encapsulated in landslide deposits of Oregon, USA
LGM to Holocene transition in the Great Lakes Area
Floating Larch Tree-Ring Chronologies from Archaeological Timbers in the Russian Altai Between about 800 BC and AD 800
We obtained over 200 archaeological wood specimens from the southeastern part of the Altai Mountains (Russia) to establish accurate calendar dates of the timbers using both radiocarbon and tree-ring analyses. Most timbers came from small and elite tombs of the Pazyryk culture (Siberian Scythians of the Iron Age period). Timbers from Hun-Sarmatian and Turk times (1st millennium AD) were studied for the first time. Three floating tree-ring width ch…
More Rapid 14 C Excursions in the Tree-Ring Record
Two radiocarbon ( 14 C) excursions are caused by an increase of incoming cosmic rays on a short time scale found in the Late Holocene (AD 774–775 and AD 993–994), which are widely explained as due to extreme solar proton events (SPE). In addition, a larger event has also been reported at 5480 BC (Miyake et al. 2017a), which is attributed to a special mode of a grand solar minimum, as well as another at 660 BC (Park et al. 2017). Clearly, other ev…
Floating Larch Tree-Ring Chronologies from Archaeological Timbers in the Russian Altai Between about 800 BC and AD 800
We obtained over 200 archaeological wood specimens from the southeastern part of the Altai Mountains (Russia) to establish accurate calendar dates of the timbers using both radiocarbon and tree-ring analyses. Most timbers came from small and elite tombs of the Pazyryk culture (Siberian Scythians of the Iron Age period). Timbers from Hun-Sarmatian and Turk times (1st millennium AD) were studied for the first time. Three floating tree-ring width ch…
Radiocarbon and Tree-Ring Dates of the Bes-Shatyr #3 Saka Kurgan in the Semirechiye, Kazakhstan
This study employs tree-ring crossdating and radiocarbon measurements to determine the precise calendar age of the Bes-Shatyr Saka necropolis (43°47′N, 81°21′E) built for wealthy tribe leaders in the Ili River Valley (Semirechiye), southern Kazakhstan. We developed a 218-yr tree-ring chronology and a highly resolved sequence of 14 C from timbers of Bes-Shatyr kurgan #3. A 4-decadal-point 14 C wiggle dates the Bes-Shatyr necropolis to 600 cal BC. …
Floating Larch Tree-Ring Chronologies from Archaeological Timbers in the Russian Altai Between about 800 BC and AD 800
We obtained over 200 archaeological wood specimens from the southeastern part of the Altai Mountains (Russia) to establish accurate calendar dates of the timbers using both radiocarbon and tree-ring analyses. Most timbers came from small and elite tombs of the Pazyryk culture (Siberian Scythians of the Iron Age period). Timbers from Hun-Sarmatian and Turk times (1st millennium AD) were studied for the first time. Three floating tree-ring width ch…
Impacts of cooling climate on prehistoric herding and farming strategies during the Bronze-Iron Age transition on the margins of the Eurasian steppe
High-resolution terrestrial MIS3 environment from trees encapsulated in landslide deposits of Oregon, USA
LGM to Holocene transition in the Great Lakes Area
Radiocarbon and Tree-Ring Dates of the Bes-Shatyr #3 Saka Kurgan in the Semirechiye, Kazakhstan
This study employs tree-ring crossdating and radiocarbon measurements to determine the precise calendar age of the Bes-Shatyr Saka necropolis (43°47′N, 81°21′E) built for wealthy tribe leaders in the Ili River Valley (Semirechiye), southern Kazakhstan. We developed a 218-yr tree-ring chronology and a highly resolved sequence of 14 C from timbers of Bes-Shatyr kurgan #3. A 4-decadal-point 14 C wiggle dates the Bes-Shatyr necropolis to 600 cal BC. …
Deglacial Hydroclimate of Midcontinental North America
During the last deglaciation temperatures over midcontinental North America warmed dramatically through the Bølling-Allerød, underwent a cool period associated with the Younger-Dryas and then reverted to warmer, near modern temperatures during the early Holocene. However, paleo proxy records of the hydroclimate of this period have presented divergent evidence. We reconstruct summer relative humidity (RH) across the last deglacial period using a m…
Ancient human genomes from across the Eurasian steppes
More Rapid 14 C Excursions in the Tree-Ring Record
Two radiocarbon ( 14 C) excursions are caused by an increase of incoming cosmic rays on a short time scale found in the Late Holocene (AD 774–775 and AD 993–994), which are widely explained as due to extreme solar proton events (SPE). In addition, a larger event has also been reported at 5480 BC (Miyake et al. 2017a), which is attributed to a special mode of a grand solar minimum, as well as another at 660 BC (Park et al. 2017). Clearly, other ev…
In Memoriam Stepan G. Shiyatov 1933–2021
Geography (8 works) · Archaeology and ancient environmental studies (5 works) · Dendrochronology (5 works) · Geology (5 works) · Geology and Paleoclimatology Research (5 works) · Physical geography (5 works) · Paleontology (4 works) · Tree-ring climate responses (4 works) · Archaeology (3 works) · Holocene (3 works)