Alexander A Prokopenko
Dados Biográficos
| ID | 5643264 |
|---|---|
| NOME | Alexander A Prokopenko |
| PRENOMES | Alexander A |
| SOBRENOME | Prokopenko |
| ASSINATURA | PROKOPENKO A A |
| AFILIAÇÕES | University of South Carolina |
| ORCID | 0000-0001-8722-4418 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 17 |
| TOTAL DE CITAÇÕES | 1 |
| TOTAL COMO AUTOR | 17 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1998 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2010 |
| ÍNDICE H | 1 |
Plio-Pleistocene transition in the continental record from Lake Baikal
Climate signals in sediment mineralogy of Lake Baikal and Lake Hovsgol during the LGM-Holocene transition and the 1-Ma carbonate record from the HDP-04 drill core
Diatom record from Lake Hovsgol, Mongolia, during the last 1Ma
Lake Hovsgol basin as a new study site for long continental paleoclimate records in continental interior Asia
Carbonate stable isotope signals in the 1-Ma sedimentary record of the HDP-04 drill core from Lake Hovsgol, NW Mongolia
Paleoenvironmental proxy records from Lake Hovsgol, Mongolia, and a synthesis of Holocene climate change in the Lake Baikal watershed
Here we discuss paleoenvironmental evolution in the Baikal region during the Holocene using new records of aquatic (diatom) and terrestrial vegetation changes from Hovsgol, Mongolia's largest and deepest lake. We reconcile previous contradictory Baikal timescales by constraining reservoir corrections of AMS dates on bulk sedimentary organic carbon. Synthesis of the Holocene records in the Baikal watershed reveals a northward progression in landsc…
Diatom biostratigraphy of Lake Baikal during the past 1.25Ma
Basin-wide sedimentation changes and deglacial lake-level rise in the Hovsgol basin, NW Mongolia
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 …
On the Nature of the Link between the Lake Baikal Biogenic Silica Record and Regional Climate Change in Siberia
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
Lake Baikal and surrounding regions
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…
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
Lake Baikal and surrounding regions
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 …
On the Nature of the Link between the Lake Baikal Biogenic Silica Record and Regional Climate Change in Siberia
Diatom biostratigraphy of Lake Baikal during the past 1.25Ma
Basin-wide sedimentation changes and deglacial lake-level rise in the Hovsgol basin, NW Mongolia
Paleoenvironmental proxy records from Lake Hovsgol, Mongolia, and a synthesis of Holocene climate change in the Lake Baikal watershed
Here we discuss paleoenvironmental evolution in the Baikal region during the Holocene using new records of aquatic (diatom) and terrestrial vegetation changes from Hovsgol, Mongolia's largest and deepest lake. We reconcile previous contradictory Baikal timescales by constraining reservoir corrections of AMS dates on bulk sedimentary organic carbon. Synthesis of the Holocene records in the Baikal watershed reveals a northward progression in landsc…
Climate signals in sediment mineralogy of Lake Baikal and Lake Hovsgol during the LGM-Holocene transition and the 1-Ma carbonate record from the HDP-04 drill core
Diatom record from Lake Hovsgol, Mongolia, during the last 1Ma
Lake Hovsgol basin as a new study site for long continental paleoclimate records in continental interior Asia
Carbonate stable isotope signals in the 1-Ma sedimentary record of the HDP-04 drill core from Lake Hovsgol, NW Mongolia
Plio-Pleistocene transition in the continental record from Lake Baikal
Geology and Paleoclimatology Research (15 obras) · Geology (12 obras) · Paleontology (12 obras) · Glacial period (9 obras) · Climate change (8 obras) · Interglacial (8 obras) · Oceanography (8 obras) · Diatom (7 obras) · Paleoclimatology (7 obras) · Physical geography (7 obras)