Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #173386:
- #173386
Main publication details
MARC recordКриохроны и термохроны юга Сибири за последние 5 миллионов лет: палеогеокриологическая интерпретация результатов исследований донных осадков озера Байкал
| Title: | Криохроны и термохроны юга Сибири за последние 5 миллионов лет: палеогеокриологическая интерпретация результатов исследований донных осадков озера Байкал |
| Title, transliterated: | Kriokhrony i termokhrony i︠u︡ga Sibiri za poslednie 5 millionov let: paleogeokriologicheskai︠a︡ interpretat︠s︡ii︠a︡ rezulʹtatov issledovaniĭ donnykh osadkov ozera Baĭkal / S.M. Fotiev. |
| Translated title: | Cryochrons and thermochrons of southern Siberia during the last 5 million years: paleogeocryological intepretation of the results of Baikal lake bottom deposit researches. |
| Author(s): | Fotiev, S. M. Fotiėv, S. M. |
| Date: | 2005. |
| Language: | Russian. |
| In: | Kriosfera Zemli. (2005.), Vol. 9(1) (2005) |
| Abstract: | Analyzes and interprets unique continuous diatom and biogenic silica traces obtained from Baikal lake bottom deposits. Reveals rhythmic alternation of cold and warm epochs. First cold epoch (3.10-3.08 Myr) was least cold and32.26 shortest. Second (2.82-2.47 Myr) saw uninterrupted severe geocryological conditions. Third (1.92-0.00 Myr) saw multiple alternation of cryochrons and thermochrons; cryogenic strata formed in cryochrons degraded completely during subsequent thermochrons. Revises palaeogeocryological history of southern Siberia through Late Pliocene and Pleistocene. Beginning of first Pleistocene cryogenic epoch in southern Siberia (3.1 Myr ago) coincides with beginning of persistent climate cooling in water area of Pacific Ocean, suggesting indivisible global Pliocene-Pleistocene cooling. |
| Notes: | Kriosfera Zemli. Vol. 9(1) :13-27 (2005). English abstract. |
| Keywords: | 551.583.3 -- Climatic changes, Quaternary. 556.54 -- River mouths, deltas and estuaries: Baikal. 551.34 -- Geocryology. Frozen ground. 556.555.6 -- Lakes, sediments. 551.7 -- Stratigraphy. 551.791 -- Pleistocene. 551.782.2 -- Pliocene. 551.336 -- Ice ages. 551.46 -- Oceanography, physical. E8 -- Glaciology: frost action and permafrost. (*501) -- Russia (Federation). (*501.1) -- European Russia. (*501.2) -- West Siberia. (*532.6) -- Respublika Buryatiya. (*66) -- North Pacific Ocean. |
| SPRI record no.: | 173386 |
LDR 03133naa#a2200000#a#4500 001 SPRI-173386 005 20231001201414.0 007 ta 008 231001s2005####xx#a##|##|###|0||#0|rus#d 035 ## ‡aSPRI-173386 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aFotiev, S. M. 242 10 ‡aCryochrons and thermochrons of southern Siberia during the last 5 million years :‡bpaleogeocryological intepretation of the results of Baikal lake bottom deposit researches.‡yeng 245 10 ‡6880-02‡aKriokhrony i termokhrony i︠u︡ga Sibiri za poslednie 5 millionov let :‡bpaleogeokriologicheskai︠a︡ interpretat︠s︡ii︠a︡ rezulʹtatov issledovaniĭ donnykh osadkov ozera Baĭkal /‡cS.M. Fotiev. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2005. 300 ## ‡ap. 13-27 :‡bdiags. 500 ## ‡aKriosfera Zemli. Vol. 9(1) :13-27 (2005). 500 ## ‡aEnglish abstract. 520 3# ‡aAnalyzes and interprets unique continuous diatom and biogenic silica traces obtained from Baikal lake bottom deposits. Reveals rhythmic alternation of cold and warm epochs. First cold epoch (3.10-3.08 Myr) was least cold and32.26 shortest. Second (2.82-2.47 Myr) saw uninterrupted severe geocryological conditions. Third (1.92-0.00 Myr) saw multiple alternation of cryochrons and thermochrons; cryogenic strata formed in cryochrons degraded completely during subsequent thermochrons. Revises palaeogeocryological history of southern Siberia through Late Pliocene and Pleistocene. Beginning of first Pleistocene cryogenic epoch in southern Siberia (3.1 Myr ago) coincides with beginning of persistent climate cooling in water area of Pacific Ocean, suggesting indivisible global Pliocene-Pleistocene cooling. 546 ## ‡aIn Russian. 546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation. 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a556.54 -- River mouths, deltas and estuaries: Baikal.‡2udc 650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a556.555.6 -- Lakes, sediments.‡2udc 650 07 ‡a551.7 -- Stratigraphy.‡2udc 650 07 ‡a551.791 -- Pleistocene.‡2udc 650 07 ‡a551.782.2 -- Pliocene.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(*501) -- Russia (Federation).‡2udc 651 #7 ‡a(*501.1) -- European Russia.‡2udc 651 #7 ‡a(*501.2) -- West Siberia.‡2udc 651 #7 ‡a(*532.6) -- Respublika Buryatiya.‡2udc 651 #7 ‡a(*66) -- North Pacific Ocean.‡2udc 700 1# ‡6880-03‡aFotiėv, S. M.‡g(alternative name) 773 0# ‡6880-04‡7nnas ‡tKriosfera Zemli. ‡gVol. 9(1) (2005) ‡wSPRI-145770 880 1# ‡6100-01/(N‡aФотиев, С. М. 880 10 ‡6245-02/(N‡aКриохроны и термохроны юга Сибири за последние 5 миллионов лет :‡bпалеогеокриологическая интерпретация результатов исследований донных осадков озера Байкал /‡cС.М. Фотиев. 880 1# ‡6700-03/(N‡aФотиэв, С. М.‡g(alternative name) 880 0# ‡6773-04/(N‡7nnas ‡tКриосфера Земли. ‡gVol. 9(1) (2005) ‡wSPRI-145770 916 ## ‡a2005/09/10 -- RF 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231001 ‡bRF