Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction

To develop multi-century stable isotope chronologies from tree rings, pooling techniques are applied to reduce laboratory costs and time. However, pooling of wood samples from different trees may have adverse effects on the signal amplitude in the final isotope chronology. We tested different poolin...

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Main Authors: Zeynab Foroozan, Jussi Grießinger, Kambiz Pourtahmasi, Achim Bräuning
Format: Article
Language:English
Published: MDPI AG 2019-06-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/9/6/270
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author Zeynab Foroozan
Jussi Grießinger
Kambiz Pourtahmasi
Achim Bräuning
author_facet Zeynab Foroozan
Jussi Grießinger
Kambiz Pourtahmasi
Achim Bräuning
author_sort Zeynab Foroozan
collection DOAJ
description To develop multi-century stable isotope chronologies from tree rings, pooling techniques are applied to reduce laboratory costs and time. However, pooling of wood samples from different trees may have adverse effects on the signal amplitude in the final isotope chronology. We tested different pooling approaches to identify the method that is most cost-efficient, without compromising the ability of the final chronology to reflect long-term climate variability as well as climatic extreme years. As test material, we used &#948;<sup>18</sup>O data from juniper trees (<i>Juniperus polycarpus</i>) from Northern Iran. We compared inter-tree and shifted 5-year blocks serial pooling of stable isotope series from 5 individual trees and addition of one single series to a shifted serial pooled chronology. The inter-tree pooled chronology showed the strongest climate sensitivity and most synchronous &#948;<sup>18</sup>O variations with the individual tree ring analyses, while the shifted block chronologies showed a marked decline in high-frequency signals and no correlations with climate variables of the growth year. Combinations of block-pooled and single isotope series compensated the high-frequency decline but added tree-individual climatic signals. Therefore, we recommend pooling calendar synchronous tree rings from individual trees as a viable alternative to individual-tree isotope measurements for robust paleoclimate reconstructions.
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spelling doaj.art-1fb0c80baeeb485eaa09628bee0da7342022-12-22T00:39:43ZengMDPI AGGeosciences2076-32632019-06-019627010.3390/geosciences9060270geosciences9060270Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate ReconstructionZeynab Foroozan0Jussi Grießinger1Kambiz Pourtahmasi2Achim Bräuning3Institute of Geography, Friedrich-Alexander-University Erlangen-Nürnberg, 91054 Erlangen, GermanyInstitute of Geography, Friedrich-Alexander-University Erlangen-Nürnberg, 91054 Erlangen, GermanyDepartment of Wood and Paper Science &amp; Technology, Faculty of Natural Resources, University of Tehran, Karaj 31587-77871, IranInstitute of Geography, Friedrich-Alexander-University Erlangen-Nürnberg, 91054 Erlangen, GermanyTo develop multi-century stable isotope chronologies from tree rings, pooling techniques are applied to reduce laboratory costs and time. However, pooling of wood samples from different trees may have adverse effects on the signal amplitude in the final isotope chronology. We tested different pooling approaches to identify the method that is most cost-efficient, without compromising the ability of the final chronology to reflect long-term climate variability as well as climatic extreme years. As test material, we used &#948;<sup>18</sup>O data from juniper trees (<i>Juniperus polycarpus</i>) from Northern Iran. We compared inter-tree and shifted 5-year blocks serial pooling of stable isotope series from 5 individual trees and addition of one single series to a shifted serial pooled chronology. The inter-tree pooled chronology showed the strongest climate sensitivity and most synchronous &#948;<sup>18</sup>O variations with the individual tree ring analyses, while the shifted block chronologies showed a marked decline in high-frequency signals and no correlations with climate variables of the growth year. Combinations of block-pooled and single isotope series compensated the high-frequency decline but added tree-individual climatic signals. Therefore, we recommend pooling calendar synchronous tree rings from individual trees as a viable alternative to individual-tree isotope measurements for robust paleoclimate reconstructions.https://www.mdpi.com/2076-3263/9/6/270tree ringsstable oxygen isotopespooling strategiesdendroclimatologyIran
spellingShingle Zeynab Foroozan
Jussi Grießinger
Kambiz Pourtahmasi
Achim Bräuning
Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction
Geosciences
tree rings
stable oxygen isotopes
pooling strategies
dendroclimatology
Iran
title Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction
title_full Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction
title_fullStr Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction
title_full_unstemmed Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction
title_short Evaluation of Different Pooling Methods to Establish a Multi-Century δ<sup>18</sup>O Chronology for Paleoclimate Reconstruction
title_sort evaluation of different pooling methods to establish a multi century δ sup 18 sup o chronology for paleoclimate reconstruction
topic tree rings
stable oxygen isotopes
pooling strategies
dendroclimatology
Iran
url https://www.mdpi.com/2076-3263/9/6/270
work_keys_str_mv AT zeynabforoozan evaluationofdifferentpoolingmethodstoestablishamulticenturydsup18supochronologyforpaleoclimatereconstruction
AT jussigrießinger evaluationofdifferentpoolingmethodstoestablishamulticenturydsup18supochronologyforpaleoclimatereconstruction
AT kambizpourtahmasi evaluationofdifferentpoolingmethodstoestablishamulticenturydsup18supochronologyforpaleoclimatereconstruction
AT achimbrauning evaluationofdifferentpoolingmethodstoestablishamulticenturydsup18supochronologyforpaleoclimatereconstruction