SwePub
Sök i LIBRIS databas

  Utökad sökning

WFRF:(Kaushal Sujay S.)
 

Sökning: WFRF:(Kaushal Sujay S.) > (2013) > Stratigraphic expre...

Stratigraphic expressions of the Holocene-Anthropocene transition revealed in sediments from remote lakes

Wolfe, Alexander P. (författare)
Hobbs, William O. (författare)
Birks, Hilary H. (författare)
visa fler...
Briner, Jason P. (författare)
Holmgren, Sofia (författare)
Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science
Ingolfsson, Olafur (författare)
Kaushal, Sujay S. (författare)
Miller, Gifford H. (författare)
Pagani, Mark (författare)
Saros, Jasmine E. (författare)
Vinebrooke, Rolf D. (författare)
visa färre...
 (creator_code:org_t)
Elsevier BV, 2013
2013
Engelska.
Ingår i: Earth-Science Reviews. - : Elsevier BV. - 1872-6828 .- 0012-8252. ; 116, s. 17-34
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Stratigraphic boundaries are ideally defined by distinct lithological, geochemical, and palaeobiological signatures, to which a chronological framework can be applied. We present a range of observations that illustrate how the Holocene-Anthropocene transition meets these criteria in its expression in sediments from remote arctic and alpine lakes, removed from direct, catchment-scale, anthropogenic influences. In glaciated lake basins, the retreat of glaciers commonly leads to lithological successions from proglacial clastic sedimentation to non-glacial organic deposition. Sediments from the majority of lakes record marked depletions in the nitrogen stable isotopic composition of sediment organic matter, reflecting anthropogenic influences on the global nitrogen cycle. In all cases, siliceous microfossil assemblages (diatoms and chrysophytes) change markedly and directionally, with regional nuances. These stratigraphic fingerprints begin to appear in the sediment record after AD 1850, but accelerate in pulses between AD 1950 and 1970 and again after AD 1980. Our review indicates that recent environmental changes associated with humankind's dominance of key global biogeochemical cycles are sufficiently pervasive to be imprinted on the sediment record of remote lakes. Moreover, these changes are of sufficient magnitude to conclude that the Holocene has effectively ended, and that the concept of Anthropocene more aptly describes current planetary dynamics. The synthesis of these observations pertains directly to ongoing discussions concerning the eventual formalization of a new stratigraphic boundary. (c) 2012 Elsevier B.V. All rights reserved.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Nyckelord

Anthropocene
Holocene
Diatoms
Nitrogen stable isotopes
Palaeolimnology

Publikations- och innehållstyp

art (ämneskategori)
ref (ämneskategori)

Hitta via bibliotek

Till lärosätets databas

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy