SwePub
Sök i LIBRIS databas

  Utökad sökning

WFRF:(Salehi Alireza)
 

Sökning: WFRF:(Salehi Alireza) > Influence of the La...

Influence of the Late Quaternary climate on sedimentology of the Jazmurian Playa, SE Iran

Sharifi-Yazdi, Masoud (författare)
Univ Tehran, Iran
Tavakoli, Vahid (författare)
Univ Tehran, Iran
Salehi-Noparvar, Sara (författare)
Univ Tehran, Iran
visa fler...
Vaezi, Alireza (författare)
Geol Survey Iran, Iran; Res Inst Earth Sci, Iran
Beni, Abdolmajid Naderi (författare)
Iranian Natl Inst Oceanog & Atmospher Sci INIOAS, Iran
Nazemi, Maziyar (författare)
Simon Fraser Univ, Canada
Duttagupta, Srimanti (författare)
San Diego State Univ, CA 92182 USA
Routh, Joyanto, 1968- (författare)
Linköpings universitet,Tema Miljöförändring,Filosofiska fakulteten
visa färre...
 (creator_code:org_t)
2022-04-02
2022
Engelska.
Ingår i: Journal of Paleolimnology. - : SPRINGER. - 0921-2728 .- 1573-0417. ; 68, s. 169-187
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Jazmurian Playa in southeast Iran is a sediment archive that has preserved a record of climate and environmental changes since the late Pleistocene. The late Pleistocene was dominated by sub-arid to arid climate interspersed with short periods of warm and humid conditions that impacted the vegetation cover and landscape. This study used sedimentological variations in a sediment core, supported by geochemical and mineralogical characteristics, to reconstruct climate change impacts and water-level fluctuations in the playa. These changes were inferred using grain-size data, magnetic susceptibility, total organic matter content, carbonate content, elemental concentrations, and mineralogical composition in a C-14-dated sediment core. Based on the inferred water level fluctuations in the playa, the core was divided into two major units. Unit 2 belonged to the late Pleistocene, characterized by a cold and dry climate. In contrast, Unit 1 was deposited during the Holocene, a time marked by prevailing warm and humid conditions, with short periods of intense dust storms. Since the late Holocene, the IOSM (Indian Ocean Summer Monsoon) has played a dominant role in regional climate. Water-level fluctuations related to humidity significantly influenced the sedimentological variables, including grain-size distribution, sorting, skewness, and roundness. During cold and arid conditions, the water level was low, and coarse sediments were deposited in the playa, with low organic matter content, low concentrations of Cu, Mn, P, and V, and evaporite minerals. In contrast, high organic matter content, presence of illite, and high concentrations of Cu, Mn, P, and V and low values of ICV (Index of Compositional Variability) imply a warm and humid climate during the Holocene. The paleoclimate reconstruction in the playa provides evidence about ongoing changes that are closely related to the paleohydrological conditions in this region.

Ämnesord

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

Nyckelord

Climate change; Playa; Elemental analyses; Water level; Magnetic susceptibility; Total organic matter

Publikations- och innehållstyp

ref (ämneskategori)
art (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