Geomorfologiâ i paleogeografiâGeomorfologiâ i paleogeografiâГеоморфология и палеогеография2949-17892949-1797The Russian Academy of Sciences68234910.31857/S2949178924040117FFCQTJHOLOCENE PALAEOGEOGRAPHYПАЛЕОГЕОГРАФИЯ ГОЛОЦЕНАResearch ArticleVegetation and climate changes in the north of the central Kamchatka depression in the late HoloceneИзменения растительности и климата Севера центральной Камчатской депрессии в позднем голоценеMukhametshinaE. O.МухаметшинаЕ. О.
Russian Federation
eomukhametshina@igras.ruShchekleinaM. D.ЩеклеинаМ. Д.
Russian Federation
eomukhametshina@igras.ruZakharovA. L.ЗахаровА. Л.
Russian Federation
eomukhametshina@igras.ruInstitute of geography RASИнститут географии РАНGeological institute RASГеологический институт РАНFersman Mineralogical MuseumМинералогический музей имени А.Е. Ферсмана РАН1512202455417719103062025Copyright ©; 2024, Russian Academy of SciencesCopyright ©; 2024, Российская академия наук2024Russian Academy of SciencesРоссийская академия наукhttps://journals.eco-vector.com/2949-1789/article/view/682349

In order to study the vegetation history of the northern part of the Central Kamchatka Depression, a core Kich was obtained and studied by lithological, tephrochronological, palynological analyses and radiocarbon dating. Palynological data allowed us to identify the main stages in the vegetation and climate development over the past 3000 years. By the end of the cool period at ~2.5 cal. kyr BP, in the Kich River valley poplar forests were replaced by alder, willow and stone birch forests. About 1.9 cal. kyr BP, sedge-dominated mire was replaced by grass meadows as a result of a series of the Shiveluch volcano eruptions and climate changes. As climate became drier stone birch forests spread about 1.2 cal. kyr BP. Since 0.8 cal. kyr BP, the areas of coniferous forests increase, first with the spread of larch and later spruce.

Спорово-пыльцевой анализ разреза Кич в северной части Центральной Камчатской депрессии, дополненный данными литологического, тефрохронологического анализов и радиоуглеродного датирования, позволил выделить основные этапы в развитии растительности и климата этой части полуострова за последние 3 тыс. лет. Около 2.5 тыс. л. н. пойменные тополевые леса в долине р. Кич на фоне завершения похолодания сменились ольшаниками, ивняками; распространились каменноберезняки. В западине начало формироваться низинное осоковое болото. Около 1.9 тыс. л. н. вследствие серии извержений влк. Шивелуч и снижения влажности климата распространились вейниковые луга. Около 1.2 тыс. л. н. нарастание сухости климата привело к распространению каменноберезняков. Около 0.8 тыс. л. н. увеличились площади хвойных лесов на севере Центральной Камчатской депрессии, сначала лиственничных, а затем – еловых.

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