Vegetation and environmental dynamics in the central part of the Kola Peninsula during the past 13.3 ka as reflected by ancient plant DNA on sediments from Lake Imandra

IF 2.2 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Anastasia Poliakova, Matthias Lenz, Martin Melles, Grigory Fedorov, Marie K. F. Merkel, Inger G. Alsos
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Abstract

The first high-resolution reconstruction of the vegetation and environmental changes during the last ca 13 300 cal a BP in the central part of the Kola Peninsula (NW Russia) was reconstructed based on sedimentary ancient DNA (sedaDNA) metabarcoding on sediment core Co1410 from Lake Imandra. In total, 204 taxa known from modern flora are identified. The resulting sequences were assigned to vascular plants (87%), bryophytes (12%), and algae (1%). About half (111 taxa, 49%) are identified at the species level. They belong to 150 genera and 86 families. So far, this is the most diverse and taxonomically detailed palaeoflora described for the Late Pleistocene–Holocene of the Kola Peninsula and North-European Russia. SedaDNA studies suggest that the vegetation cover in the region developed from (1) plant colonisation of the study area after the glacier retreated during the Allerød warming at ca 13 300–13 000 a BP to (2) Younger Dryas cold period with re-entering of the glaciers in the catchment of the Grater (Bolshaya) Imandra and establishing of the steppe–tundra communities. (3) Warming and increasing in vegetation diversity during the Early Holocene, with the formation of the birch forests by the end of this time zone. (4) Mid-Holocene temperature maximum is correlated with the highest regional plant diversity and a pronounced role of the thermophilic taxa, that is, Lonicera species, Prunus padus, Populus tremula, Sorbus sp./Cotoneaster sp. The highest so far revealed regional diversity of the higher spore plants (10) and aquatic plants (23) is evidenced. Mixed deciduous and coniferous forests were established in the research area during this period, and a drop in plant diversity occurred afterwards. (5) During the Late Holocene, modern communities are formed with a slight increase in biodiversity because of increasing input from cultural plants and weeds. Human impact is clearly diagnosed after 250 a BP, indicated by the presence of Ribes sp., Hypericum sp., and Mentha arvensis as well as eutrophic weeds, that is, Trifolium sp. and Urtica dioica. In addition, this study revealed the past dynamics of some plants rare for the Murmansk region, namely Pteridium aquilinum, with its maximum of occurrence at ca 11 000–8000 cal a BP and a strong decrease thereafter, and Nuphar sp./Nymphaea sp. occurring regularly since ca 7700 cal a BP and eliminating from the record after ca 3500 cal a BP.

Abstract Image

伊曼德拉湖沉积物古植物DNA反映的科拉半岛中部过去13.3 ka的植被和环境动态
利用伊曼德拉湖Co1410沉积古DNA元条形码技术,对俄罗斯西北部科拉半岛中部近13 ~ 300 cal a BP植被和环境变化进行了首次高分辨率重建。共鉴定出204个已知的现代植物区系。得到的序列分别属于维管植物(87%)、苔藓植物(12%)和藻类(1%)。大约一半(111个分类群,49%)在物种水平上得到鉴定。它们分属86科150属。到目前为止,这是对科拉半岛和俄罗斯北欧地区晚更新世-全新世最多样化和分类最详细的古植物群描述。SedaDNA研究表明,该地区的植被覆盖经历了(1)约13300 - 13000 a BP的Allerød变暖期间冰川退缩后的植物定植,(2)新Dryas寒期冰川重新进入Grater (Bolshaya) Imandra集水区,建立了草原-苔原群落。(3)全新世早期气候变暖,植被多样性增加,白桦林在该时区末形成。(4)中全新世最高温度与区域植物多样性最高相关,且嗜热分类群Lonicera、Prunus padus、Populus tremula、Sorbus sp./Cotoneaster sp.的作用显著,其中高孢子植物(10)和水生植物(23)的区域多样性最高。这一时期研究区形成了落叶针叶林混交林,之后植物多样性下降。(5)在全新世晚期,由于外来植物和杂草的输入增加,现代群落形成,生物多样性略有增加。人类的影响在250a BP后被明确诊断出来,由Ribes sp.、Hypericum sp.、Mentha arvensis以及富营养化杂草(即Trifolium sp.和Urtica dioica)的存在表明。此外,该研究还揭示了摩尔曼斯克地区罕见植物翼蕨(Pteridium aquilinum)的历史动态,其在11000 ~ 8000cal a BP之间最高,此后急剧减少;Nuphar sp./Nymphaea sp.在7700 cal a BP之后有规律地出现,在3500 cal a BP之后就消失了。
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来源期刊
Journal of Quaternary Science
Journal of Quaternary Science 地学-地球科学综合
CiteScore
4.70
自引率
8.70%
发文量
82
审稿时长
6-12 weeks
期刊介绍: The Journal of Quaternary Science publishes original papers on any field of Quaternary research, and aims to promote a wider appreciation and deeper understanding of the earth''s history during the last 2.58 million years. Papers from a wide range of disciplines appear in JQS including, for example, Archaeology, Botany, Climatology, Geochemistry, Geochronology, Geology, Geomorphology, Geophysics, Glaciology, Limnology, Oceanography, Palaeoceanography, Palaeoclimatology, Palaeoecology, Palaeontology, Soil Science and Zoology. The journal particularly welcomes papers reporting the results of interdisciplinary or multidisciplinary research which are of wide international interest to Quaternary scientists. Short communications and correspondence relating to views and information contained in JQS may also be considered for publication.
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