Eastern Mediterranean hydroclimate over the late glacial and Holocene, reconstructed from the sediments of Nar lake, central Turkey, using stable isotopes and carbonate mineralogy

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Eastern Mediterranean hydroclimate over the late glacial and Holocene, reconstructed from the sediments of Nar lake, central Turkey, using stable isotopes and carbonate mineralogy. / Dean, Jonathan R.; Jones, Matthew D.; Noble, Stephen R.; Eastwood, Warren J.; Leng, Melanie J.; Metcalfe, Sarah E.; Sloane, Hilary J.; Sahy, Diana; Roberts, C. Neil.

In: Quaternary Science Reviews, Vol. 124, 15.09.2015, p. 162-174.

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Dean, Jonathan R. ; Jones, Matthew D. ; Noble, Stephen R. ; Eastwood, Warren J. ; Leng, Melanie J. ; Metcalfe, Sarah E. ; Sloane, Hilary J. ; Sahy, Diana ; Roberts, C. Neil. / Eastern Mediterranean hydroclimate over the late glacial and Holocene, reconstructed from the sediments of Nar lake, central Turkey, using stable isotopes and carbonate mineralogy. In: Quaternary Science Reviews. 2015 ; Vol. 124. pp. 162-174.

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@article{84066aadaa114a9aa8ed883bf2b31e6b,
title = "Eastern Mediterranean hydroclimate over the late glacial and Holocene, reconstructed from the sediments of Nar lake, central Turkey, using stable isotopes and carbonate mineralogy",
abstract = "There is a lack of high-resolution records of hydroclimate variability in the Eastern Mediterranean from the late glacial and early Holocene. More knowledge of the speed of climate shifts and the degree to which they were synchronous with changes in the North Atlantic or elsewhere is required to understand better the controls on Eastern Mediterranean climate. Using endogenic carbonate from a sediment sequence from Nar G{\"o}l{\"u}, a maar lake in central Turkey, dated by varve counting and uranium-thorium methods, we present high-resolution (∼25 years) oxygen (δ18O) and carbon isotope records, supported by carbonate mineralogy data, spanning the late glacial and Holocene. δ18Ocarbonate at Nar G{\"o}l{\"u} has been shown previously to be a strong proxy for regional water balance. After a dry period (i.e. evaporation far exceeding precipitation) in the Younger Dryas, the data show a transition into the relatively wetter early Holocene. In the early Holocene there are two drier periods that appear to peak at ∼9.3 ka and ∼8.2 ka, coincident with cooling {\textquoteleft}events{\textquoteright} seen in North Atlantic records. After this, and as seen in other records from the Eastern Mediterranean, there is a millennial-scale drying trend through the Mid Holocene Transition. The relatively dry late Holocene is punctuated by centennial-scale drought intervals, at the times of 4.2 ka {\textquoteleft}event{\textquoteright} and Late Bronze Age societal {\textquoteleft}collapse{\textquoteright}. Overall, we show that central Turkey is drier when the North Atlantic is cooler, throughout this record and at multiple timescales, thought to be due to a weakening of the westerly storm track resulting from reduced cyclogenesis in the North Atlantic. However, some features, such as the Mid Holocene Transition and the fact the early Holocene dry episodes at Nar G{\"o}l{\"u} are of a longer duration than the more discrete {\textquoteleft}events{\textquoteright} seen in North Atlantic records, imply there are additional controls on Eastern Mediterranean hydroclimate.",
keywords = "Oxygen and carbon isotopes, Eastern Mediterranean, Lake sediment, Holocene, Late glacial, Mid Holocene transition, 9.3 ka event, 8.2 ka event, 4.2 ka event, Late Bronze Age",
author = "Dean, {Jonathan R.} and Jones, {Matthew D.} and Noble, {Stephen R.} and Eastwood, {Warren J.} and Leng, {Melanie J.} and Metcalfe, {Sarah E.} and Sloane, {Hilary J.} and Diana Sahy and Roberts, {C. Neil}",
year = "2015",
month = sep
day = "15",
doi = "10.1016/j.quascirev.2015.07.023",
language = "English",
volume = "124",
pages = "162--174",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Eastern Mediterranean hydroclimate over the late glacial and Holocene, reconstructed from the sediments of Nar lake, central Turkey, using stable isotopes and carbonate mineralogy

AU - Dean, Jonathan R.

AU - Jones, Matthew D.

AU - Noble, Stephen R.

AU - Eastwood, Warren J.

AU - Leng, Melanie J.

AU - Metcalfe, Sarah E.

AU - Sloane, Hilary J.

AU - Sahy, Diana

AU - Roberts, C. Neil

PY - 2015/9/15

Y1 - 2015/9/15

N2 - There is a lack of high-resolution records of hydroclimate variability in the Eastern Mediterranean from the late glacial and early Holocene. More knowledge of the speed of climate shifts and the degree to which they were synchronous with changes in the North Atlantic or elsewhere is required to understand better the controls on Eastern Mediterranean climate. Using endogenic carbonate from a sediment sequence from Nar Gölü, a maar lake in central Turkey, dated by varve counting and uranium-thorium methods, we present high-resolution (∼25 years) oxygen (δ18O) and carbon isotope records, supported by carbonate mineralogy data, spanning the late glacial and Holocene. δ18Ocarbonate at Nar Gölü has been shown previously to be a strong proxy for regional water balance. After a dry period (i.e. evaporation far exceeding precipitation) in the Younger Dryas, the data show a transition into the relatively wetter early Holocene. In the early Holocene there are two drier periods that appear to peak at ∼9.3 ka and ∼8.2 ka, coincident with cooling ‘events’ seen in North Atlantic records. After this, and as seen in other records from the Eastern Mediterranean, there is a millennial-scale drying trend through the Mid Holocene Transition. The relatively dry late Holocene is punctuated by centennial-scale drought intervals, at the times of 4.2 ka ‘event’ and Late Bronze Age societal ‘collapse’. Overall, we show that central Turkey is drier when the North Atlantic is cooler, throughout this record and at multiple timescales, thought to be due to a weakening of the westerly storm track resulting from reduced cyclogenesis in the North Atlantic. However, some features, such as the Mid Holocene Transition and the fact the early Holocene dry episodes at Nar Gölü are of a longer duration than the more discrete ‘events’ seen in North Atlantic records, imply there are additional controls on Eastern Mediterranean hydroclimate.

AB - There is a lack of high-resolution records of hydroclimate variability in the Eastern Mediterranean from the late glacial and early Holocene. More knowledge of the speed of climate shifts and the degree to which they were synchronous with changes in the North Atlantic or elsewhere is required to understand better the controls on Eastern Mediterranean climate. Using endogenic carbonate from a sediment sequence from Nar Gölü, a maar lake in central Turkey, dated by varve counting and uranium-thorium methods, we present high-resolution (∼25 years) oxygen (δ18O) and carbon isotope records, supported by carbonate mineralogy data, spanning the late glacial and Holocene. δ18Ocarbonate at Nar Gölü has been shown previously to be a strong proxy for regional water balance. After a dry period (i.e. evaporation far exceeding precipitation) in the Younger Dryas, the data show a transition into the relatively wetter early Holocene. In the early Holocene there are two drier periods that appear to peak at ∼9.3 ka and ∼8.2 ka, coincident with cooling ‘events’ seen in North Atlantic records. After this, and as seen in other records from the Eastern Mediterranean, there is a millennial-scale drying trend through the Mid Holocene Transition. The relatively dry late Holocene is punctuated by centennial-scale drought intervals, at the times of 4.2 ka ‘event’ and Late Bronze Age societal ‘collapse’. Overall, we show that central Turkey is drier when the North Atlantic is cooler, throughout this record and at multiple timescales, thought to be due to a weakening of the westerly storm track resulting from reduced cyclogenesis in the North Atlantic. However, some features, such as the Mid Holocene Transition and the fact the early Holocene dry episodes at Nar Gölü are of a longer duration than the more discrete ‘events’ seen in North Atlantic records, imply there are additional controls on Eastern Mediterranean hydroclimate.

KW - Oxygen and carbon isotopes

KW - Eastern Mediterranean

KW - Lake sediment

KW - Holocene

KW - Late glacial

KW - Mid Holocene transition

KW - 9.3 ka event

KW - 8.2 ka event

KW - 4.2 ka event

KW - Late Bronze Age

U2 - 10.1016/j.quascirev.2015.07.023

DO - 10.1016/j.quascirev.2015.07.023

M3 - Article

VL - 124

SP - 162

EP - 174

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

ER -