Eugene B Karabanov
Biographic Data
| ID | 7511637 |
|---|---|
| NAME | Eugene B Karabanov |
| GIVEN NAMES | Eugene B |
| FAMILY NAME | Karabanov |
| SIGNATURE | KARABANOV E B |
| VERIFIED | No |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 7 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1998 |
| LATEST PUBLICATION YEAR | 2002 |
| H-INDEX | 0 |
The Stability and the Abrupt Ending of the Last Interglaciation in Southeastern Siberia
Paleoproductivity records from Lake Baikal indicate that the last interglaciation in southeastern Siberia lasted ca. 12,000 yr from 127,000 to 115,000 yr B.P., was punctuated by a climatic oscillation about 120,000 yr ago, and ended abruptly with a rapid onset of regional glaciation during marine isotope substage (MIS) 5d. The Siberian equivalent of the MIS 5e–5d transition appears to lead the post-Eemian cold pulses in Europe and in the central …
Biogenic Silica Record of the Lake Baikal Response to Climatic Forcing during the Brunhes
This work presents a detailed, orbitally tuned biogenic silica record of continental paleoclimate change during the Brunhes chron. The Brunhes/Matuyama boundary lies within the warm isotopic stage 19 in Baikal, and the boundaries between eight lithological cycles correspond to terminations in the marine oxygen isotope record. The high amplitude and resolution of climatically driven changes in BioSi content in Lake Baikal sediments permits tuning …
Insolation regime in Siberia as a major factor controlling diatom production in Lake Baikal during the past 800,000 years
The link between tectonic and paleoclimatic events at 2.8–2.5MaBP in the Lake Baikal region
The detailed record of climatic events during the past 75,000 yrs BP from the Lake Baikal drill core BDP-93-2
The Lake Baikal drilling project in the context of a global lake drilling initiative
Evidence from Lake Baikal for Siberian Glaciation during Oxygen-Isotope Substage 5d
The paleoclimatic record from bottom sediments of Lake Baikal (eastern Siberia) reveals new evidence for an abrupt and intense glaciation during the initial part of the last interglacial period (isotope substage 5d). This glaciation lasted about 12,000 yr from 117,000 to 105,000 yr B.P. according to correlation with the SPECMAP isotope chronology. Lithological and biogeochemical evidence of glaciation from Lake Baikal agrees with evidence for the…
No prominent works on this page.
Evidence from Lake Baikal for Siberian Glaciation during Oxygen-Isotope Substage 5d
The paleoclimatic record from bottom sediments of Lake Baikal (eastern Siberia) reveals new evidence for an abrupt and intense glaciation during the initial part of the last interglacial period (isotope substage 5d). This glaciation lasted about 12,000 yr from 117,000 to 105,000 yr B.P. according to correlation with the SPECMAP isotope chronology. Lithological and biogeochemical evidence of glaciation from Lake Baikal agrees with evidence for the…
Biogenic Silica Record of the Lake Baikal Response to Climatic Forcing during the Brunhes
This work presents a detailed, orbitally tuned biogenic silica record of continental paleoclimate change during the Brunhes chron. The Brunhes/Matuyama boundary lies within the warm isotopic stage 19 in Baikal, and the boundaries between eight lithological cycles correspond to terminations in the marine oxygen isotope record. The high amplitude and resolution of climatically driven changes in BioSi content in Lake Baikal sediments permits tuning …
Insolation regime in Siberia as a major factor controlling diatom production in Lake Baikal during the past 800,000 years
The link between tectonic and paleoclimatic events at 2.8–2.5MaBP in the Lake Baikal region
The detailed record of climatic events during the past 75,000 yrs BP from the Lake Baikal drill core BDP-93-2
The Lake Baikal drilling project in the context of a global lake drilling initiative
The Stability and the Abrupt Ending of the Last Interglaciation in Southeastern Siberia
Paleoproductivity records from Lake Baikal indicate that the last interglaciation in southeastern Siberia lasted ca. 12,000 yr from 127,000 to 115,000 yr B.P., was punctuated by a climatic oscillation about 120,000 yr ago, and ended abruptly with a rapid onset of regional glaciation during marine isotope substage (MIS) 5d. The Siberian equivalent of the MIS 5e–5d transition appears to lead the post-Eemian cold pulses in Europe and in the central …
Geology and Paleoclimatology Research (6 works) · Glacial period (5 works) · Interglacial (5 works) · Climate change (4 works) · Climatology (4 works) · Geology (4 works) · Paleoclimatology (4 works) · Paleontology (4 works) · Pleistocene-Era Hominins and Archaeology (4 works) · Diatom (3 works)