Lake development and vegetation history in coastal Primor'ye: implications for Holocene climate of the southeastern Russian Far East
Lake development and vegetation history in coastal Primor'ye: implications for Holocene climate of the southeastern Russian Far East
复制标题
滨海边疆区的湖泊发育和植被历史：对俄罗斯远东东南部全新世气候的影响
作者：
Lozhkin A
拉脱维亚湖提供了Primor‘ye东南部为数不多的高分辨率古环境记录之一。它追溯了过去8.6亿年间的盆地、植被和气候历史。拉脱维亚盆地经历了四个阶段，其中两个阶段涉及湖泊、泻湖和海湾环境之间的频繁变化(约8.6-7.0公卡)。Ka BP和C.2.1千卡。Ka BP-现在)。在7.0到6.9卡之间存在沙洲。Ka BP。拉脱维亚盆地稳定的最长间隔期为6.9-2.1千卡。Ka BP时，盆地是一个盐碱度不同的泻湖。栎类-阔叶林是过去整个地区植被的特征。喜温树种(如核桃、红穗石竹、榆树、丁香、丁香)和红松的变化反映了中全新世温度和湿度的变化。出现了一段气候最温暖的时期，大约8.6-5.1卡。Ka BP，最潮湿的条件在7.5-4.3大卡之间。Ka BP，尽管温度和降水的所有变化都是渐进的。拉脱维亚湖的研究结果表明，全新世中期至晚期气候的变化与东亚夏季风的变化关系更密切，与海平面波动的联系较小。这项调查表明，尽管滨海Primor‘ye湖泊的沉积环境不断变化，但仍能提供可靠的古植被和古气候记录。
Latvia Lake provides one of the few high‐resolution palaeoenvironmental records from southeastern Primor'ye. It traces basin, vegetation and climate histories over the pastc.8.6 ka. The Latvia basin experienced four phases, two of which involved frequent shifts amongst lake, lagoon and bay settings (c.8.6–7.0 cal. ka BP andc.2.1 cal. ka BP–present). A sandbar was present betweenc.7.0 and 6.9 cal. ka BP. The longest interval of Latvia basin stability was fromc.6.9–2.1 cal. ka BP when the basin was a lagoon of varying salinities.Quercus‐broadleaf forests characterized the regional vegetation throughout the pastc.8.6 ka. Variations in thermophilous species (e.g.Juglans,Carpinus,Ulmus,Tilia,Syringa) andPinus koraiensisreflect shifts in temperature and moisture during the Middle Holocene. A period of warmest climate occurredc.8.6–5.1 cal. ka BP with wettest conditions fromc.7.5–4.3 cal. ka BP, although all changes in temperature and precipitation were gradual. The Latvia Lake results indicate that changes in Middle to Late Holocene climates were linked more closely to shifts in the East Asian Summer Monsoon and less so to sea level oscillations. This investigation demonstrates that lakes of coastal Primor'ye can provide reliable palaeovegetation and palaeoclimate records despite their changing depositional environments.
登录
查看更多内容
全球和地方因素在决定西北太平洋南千岛群岛和科曼达尔群岛中晚期全新世环境历史中的作用
DOI：
10.1016/j.palaeo.2004.02.023
发表时间：
2004
期刊：
Palaeogeography, Palaeoclimatology, Palaeoecology
影响因子：
--
作者：
N. Razjigaeva;T. Grebennikova;L. Ganzey;L. Mokhova;V. Bazarova
通讯作者：
V. Bazarova
影响因子：
4
作者：
C. Leipe;S. Müller;Konrad Hille;Hirofumi Kato;F. Kobe;M. Schmidt;Konrad Seyffert;R. Spengler;Mayke Wagner;A. Weber;P. Tarasov
通讯作者：
C. Leipe;S. Müller;Konrad Hille;Hirofumi Kato;F. Kobe;M. Schmidt;Konrad Seyffert;R. Spengler;Mayke Wagner;A. Weber;P. Tarasov
影响因子：
3.9
作者：
L. Nazarova;Т. А. Grebennikova;N. Razjigaeva;L. Ganzey;N. Belyanina;K. Arslanov;V. Kaistrenko;А. О. Gorbunov;А. А. Kharlamov-А.;N. Rudaya;O. Palagushkina;B. Biskaborn;B. Diekmann
通讯作者：
L. Nazarova;Т. А. Grebennikova;N. Razjigaeva;L. Ganzey;N. Belyanina;K. Arslanov;V. Kaistrenko;А. О. Gorbunov;А. А. Kharlamov-А.;N. Rudaya;O. Palagushkina;B. Biskaborn;B. Diekmann
谢尔盖夫高原泥炭沼泽记录的南锡霍特-阿林中部地区自然环境的发展
影响因子：
0.8
作者：
N. G. Razzhigaeva;L. Ganzey;T. Grebennikova;L. Mokhova;T. A. Kopoteva;E. Kudryavtseva;K. Arslanov;F. Maksimov;A. Petrov;M. Klimin
通讯作者：
M. Klimin
俄罗斯远东锡霍特-阿林山什科托夫斯科高原古湖沉积物记录的全新世晚期环境变化
影响因子：
3
作者：
N. Razjigaeva;L. Ganzey;L. Mokhova;T. R. Makarova;A. Panichev;E. Kudryavtseva;K. Arslanov;F. Maksimov;A. Starikova
通讯作者：
A. Starikova