کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
8915006 | 1640754 | 2018 | 11 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Archaeal community changes in Lateglacial lake sediments: Evidence from ancient DNA
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کلمات کلیدی
Ancient DNA - DNA باستانیLast deglaciation - آخرین انفجارArchaea - باستانیان یا آرکیاLipid biomarkers - بیومارکرهای لیپیدیshotgun sequencing - ترتیب تفنگ ساچمهایSouthern Sweden - جنوب سوئدpaleoclimate - دیرینه اقلیمLake sediments - رسوبات دریاچهایMetagenomics - متاژنومیکسPaleoenvironment - محیط زیست
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
پیش نمایش صفحه اول مقاله
چکیده انگلیسی
The Lateglacial/early Holocene sediments from the ancient lake at Hässeldala Port, southern Sweden provide an important archive for the environmental and climatic shifts at the end of the last ice age and the transition into the present Interglacial. The existing multi-proxy data set highlights the complex interplay of physical and ecological changes in response to climatic shifts and lake status changes. Yet, it remains unclear how microorganisms, such as Archaea, which do not leave microscopic features in the sedimentary record, were affected by these climatic shifts. Here we present the metagenomic data set of Hässeldala Port with a special focus on the abundance and biodiversity of Archaea. This allows reconstructing for the first time the temporal succession of major Archaea groups between 13.9 and 10.8 ka BP by using ancient environmental DNA metagenomics and fossil archaeal cell membrane lipids. We then evaluate to which extent these findings reflect physical changes of the lake system, due to changes in lake-water summer temperature and seasonal lake-ice cover. We show that variations in archaeal composition and diversity were related to a variety of factors (e.g., changes in lake water temperature, duration of lake ice cover, rapid sediment infilling), which influenced bottom water conditions and the sediment-water interface. Methanogenic Archaea dominated during the Allerød and Younger Dryas pollen zones, when the ancient lake was likely stratified and anoxic for large parts of the year. The increase in archaeal diversity at the Younger Dryas/Holocene transition is explained by sediment infilling and formation of a mire/peatbog.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Quaternary Science Reviews - Volume 181, 1 February 2018, Pages 19-29
Journal: Quaternary Science Reviews - Volume 181, 1 February 2018, Pages 19-29
نویسندگان
Engy Ahmed, Laura Parducci, Per Unneberg, Rasmus Ã
gren, Frederik Schenk, Jayne E. Rattray, Lu Han, Francesco Muschitiello, Mikkel W. Pedersen, Rienk H. Smittenberg, Kweku Afrifa Yamoah, Tanja Slotte, Barbara Wohlfarth,