Subfossil Spore–Pollen Spectra of Northern Yakutia as a Key to the Interpretation of Paleoecological Studies

IF 1 4区 地球科学 Q3 GEOLOGY
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引用次数: 0

Abstract

The results of the study obtained for spores and pollen from the subfossil spectra of samples from the Bykovsky Peninsula (northern Yakutia) are presented in order to compare them with the current vegetation composition, to consider the major cryogenic disturbances of palynological remains, and to analyze their cryogenic destruction processes. The abundant alien pollen of Betula sect. Nanae and Alnus in the spectra is due to open landscapes, relatively low pollen productivity, and the transition of herbs and shrubs prevailing in the local phytocenoses to a vegetative propagation in severe climatic conditions. The selective role of cryogenesis in the spore–pollen spectra formation is related to repeated sediment thawing and freezing cycles, resulting in physical damage (ruptures and cracks) in palynological remains. The results of research contribute to the study of the methodological aspects of palynotaphonomy in cryolithic zone sediments. They can be used to reconstruct the Neopleistocene landscapes and vegetation and to study cryopreservation of fossil living organisms and their diversity in the permafrost areas.

北雅库特亚化石孢粉谱是解释古生态学研究的一把钥匙
摘要 本文介绍了从拜科夫斯基半岛(雅库特北部)样本的亚化石光谱中获得的孢子和花粉研究结果,以便将其与当前的植被组成进行比较,考虑古植物学遗迹的主要低温干扰,并分析其低温破坏过程。桦树科(Betula sect.光谱中大量的外来花粉是由于地形开阔、花粉生产力相对较低,以及当地植物区系中的草本和灌木在恶劣的气候条件下向无性繁殖过渡。低温作用在孢粉谱形成过程中的选择性作用与反复的沉积物解冻和冻结循环有关,这导致了古植物学遗迹的物理损坏(破裂和裂缝)。研究成果有助于研究冷冻区沉积物中的古植物学方法。这些成果可用于重建新始新世的地貌和植被,以及研究永冻地区生物化石的低温保存及其多样性。
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来源期刊
CiteScore
1.80
自引率
30.00%
发文量
22
审稿时长
>12 weeks
期刊介绍: Stratigraphy and Geological Correlation is the only journal that provides comprehensive coverage of the fundamental and applied aspects of stratigraphy and the correlation of geologic events and processes in time and space. Articles are based on the results of multidisciplinary studies and are for researchers, university professors, students, and geologists interested in stratigraphy and the chronological features of the world’s geological record.
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