DOI: 10.1016/j.quascirev.2015.08.005
Scopus记录号: 2-s2.0-84940109539
论文题名: Spatial and temporal variability of lake ontogeny in south-western Greenland
作者: Law A.C. ; Anderson N.J. ; McGowan S.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2015
卷: 126 起始页码: 1
结束页码: 16
语种: 英语
英文关键词: Climatic variability
; Diatom
; Greenland
; Holocene
; Low Arctic
; Ontogeny
Scopus关键词: Alkalinity
; Catchments
; Climate change
; Deposition
; Dust
; Erosion
; pH
; Runoff
; Stratigraphy
; Weathering
; Climatic variability
; Diatom
; Greenland
; Holocenes
; Low Arctic
; Ontogeny
; Lakes
; alkalinity
; carotenoid
; climate effect
; climate variation
; diatom
; erosion
; lake ecosystem
; Little Ice Age
; Medieval Warm Period
; nutrient availability
; ontogeny
; paleolimnology
; spatiotemporal analysis
; stratigraphy
; weathering
; Arctic
; Greenland
; Kangerlussuaq Fjord
; Sisimiut Harbour
; algae
; Bacillariophyta
英文摘要: Holocene palaeolimnological records of diatoms and β carotene (a proxy for aquatic production) from four lakes in the low Arctic region of south-western Greenland were used to investigate the role of climate on lake ontogeny. Two of the lakes are located in the maritime, coastal region near Sisimiut and two inland close to the head of Kangerlussuaq fjord, where there is a more continental climate. Diatom records from the four lakes (AT1, AT4, SS1381, SS8) had similar long-term ontogeny trends, independent of climatic setting and the changes are interpreted as responses to first order weathering controls on catchment/lake chemistry. Short-term excursions from these broad trends occurred in one coastal site (AT4) caused by intense erosion of the steep catchment, and at inland sites where temporary hydrological closure and lake level decline occurred during the mid-Holocene (~8000 - 5000 cal a BP). Algal production (as β carotene) was more closely and consistently correlated with climatic changes; it peaked during the mid-Holocene, the warmest period of the Holocene, at all sites and there were transient increases in production in inland lakes during the Medieval Climate Anomaly and Little Ice Age because of fertilization through increased aeolian dust deposition. A synthesis of seven palaeolimnological records from this region identified that only the mid-Holocene was correlated with diatom stratigraphic zones and there was considerable among-site variability in later Holocene lake response to climate forcing in this area. Comparable long-term trends in species assemblage turnover (DCA/CA axis 1 scores) clearly demonstrate that lakes have predictable ontogeny trends in this region, characterised by maximum alkalinity and nutrient availability in the first few millennia followed by progressive oligotrophication and alkalinity loss. However, individual lake and catchment characteristics (lake morphology, catchment geomorphology), when modified by climatic change (vegetation cover, erosion, weathering rates, aeolian dust deposition, lake level) can diverge from this ontogeny template leading to complex ecological transitions in lakes from this region. © 2015 Elsevier Ltd. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59820
Appears in Collections: 过去全球变化的重建
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作者单位: Department of Geography, Loughborough University, Loughborough, Leicestershire, United Kingdom; School of Geography, University of Nottingham, University Park, Nottingham, United Kingdom; School of Geography, University of Nottingham Malaysia Campus, Semenyih, Selangor Darul Ehsan, Malaysia
Recommended Citation:
Law A.C.,Anderson N.J.,McGowan S.. Spatial and temporal variability of lake ontogeny in south-western Greenland[J]. Quaternary Science Reviews,2015-01-01,126