Динамика субполярного оледенения за две тысячи лет по лихенометрическим данным

MARCXML

LDR 03698naa#a2200000#a#4500
001 SPRI-168394
005 20240418163522.0
007 ta
008 240418s2003####xx#ab#|##|###|0||#0|rus#d
035 ## ‡aSPRI-168394
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aSolomina, O. N.
242 10 ‡aDynamics of subpolar glaciation in the last two thousand years from lichenometry data.‡yeng
245 10 ‡6880-02‡aDinamika subpoli︠a︡rnogo oledenenii︠a︡ za dve tysi︠a︡chi let po likhenometricheskim dannym /‡cO.N. Solomina.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 17-30 :‡bdiags., table, maps.
500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 94 :17-30 (2003).
500 ## ‡aRussian summary and figure captions.
520 3# ‡aAnalyzes lichen growth curves used to date glacial landforms in 18 (sub-)polar regions. Estimates reliability of lichenometric dates and recommends improvements. Critical point of many growth curves is period from few hundred to few thousand years, where control points absent. Technique remains useful in (sub-)polar climate in absence of alternatives. (Sub-)Antarctic regions require special attention because lichen growth rates are poorly studied. Presents moraine chronologies using lichenometry, ¹⁴C and tree ring dating, tephrochronology and historical data. Argues these show glacier variations of last millennium on two hemispheres are broadly similar. Distinguishes two waves of glacier activity within Little Ice Age (LIA); first starting 700-800 years ago, and second from 17th to beginning of 20th century. Maximum glacier extents in many Arctic regions occurred later than in temperate regions. Attributes Greenland and Franz Josef Land advances during Medieval warm period to precipitation anomalies. Reports evidence of glacier advances from first millennium AD sparse, probably because of subsequent disturbance by LIA advances.
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 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡a582.29 -- Lichens.‡2udc
650 07 ‡a539.16 -- Radio-carbon dating.‡2udc
650 07 ‡a634.0.561.24 -- Dendrochronology.‡2udc
650 07 ‡a546.26 -- Carbon.‡2udc
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*527) -- Frantsa-Iosifa, Zemlya.‡2udc
651 #7 ‡a(*34) -- Jan Mayen.‡2udc
651 #7 ‡a(*35) -- Iceland.‡2udc
651 #7 ‡a(*548) -- Scandinavia.‡2udc
651 #7 ‡a(*49) -- Alaska.‡2udc
651 #7 ‡a(*531.25) -- Kamchatskaya Oblast'.‡2udc
651 #7 ‡a(234.8) -- Urals.‡2udc
651 #7 ‡a(*462) -- Baffin Island.‡2udc
651 #7 ‡a(83) -- Chile.‡2udc
651 #7 ‡a(*725) -- South Orkney Islands.‡2udc
651 #7 ‡a(*726.1) -- South Shetland Islands.‡2udc
651 #7 ‡a(*74) -- Australian Antarctic Territory.‡2udc
651 #7 ‡a(*76) -- Ross Dependency.‡2udc
773 0# ‡6880-03‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 94 (2003) ‡wSPRI-33585
880 1# ‡6100-01/(N‡aСоломина, О. Н.
880 10 ‡6245-02/(N‡aДинамика субполярного оледенения за две тысячи лет по лихенометрическим данным /‡cО.Н. Соломина.
880 0# ‡6773-03/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 94 (2003) ‡wSPRI-33585
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240418