<abstract xmlns="http://www.w3.org/1999/xhtml">A set of subfossil macroremains, consisting of 118 oak (<italic>Quercus sp</italic>.) and 61 elm (<italic>Ulmus sp</italic>.) trees, was collected at five sites in the foothills of the Eastern Carpathians along the course of the Suceava river. The tree-ring widths of the subfossil samples were measured. Dendrochronological synchronization resulted in five oak chronologies, although each encompassed relatively few (2 to 4) reliably cross-dated series. Radiocarbon analysis was performed on samples from three of the floating chronologies and on an additional single oak sample. Double radiocarbon data from two of the floating chronologies allowed for improved calibration using the wiggle-match estimate of the subfossil oak remains. Radiocarbon evidence highlighted the fact that the subfossil material recovered from the fluvial deposits of the Suceava river may represent a substantial part of the Holocene, from ~700 to ~7000 years ago. When temporal distribution of 14C dated sequences from the Suceava black oaks were compared to the calibrated age ranges reported from nearby rivers (Siret, Moldova), deposition events were observed to coincide at around 0.8–0.9 ka cal BP and ~3.7–3.6 ka cal BP. The five presented floating chronologies, and especially the first 14C wiggle-matched tree-ring sequences of Ro-manian black oaks could become key building blocks in a longer regional oak tree-ring chronology for the Eastern Carpathian region.</abstract>

A set of subfossil macroremains, consisting of 118 oak (Quercus sp.) and 61 elm (Ulmus sp.) trees, was collected at five sites in the foothills of the Eastern Carpathians along the course of the Suceava river. The tree-ring widths of the subfossil samples were measured. Dendrochronological synchronization resulted in five oak chronologies, although each encompassed relatively few (2 to 4) reliably cross-dated series. Radiocarbon analysis was performed on samples from three of the floating chronologies and on an additional single oak sample. Double radiocarbon data from two of the floating chronologies allowed for improved calibration using the wiggle-match estimate of the subfossil oak remains. Radiocarbon evidence highlighted the fact that the subfossil material recovered from the fluvial deposits of the Suceava river may represent a substantial part of the Holocene, from ~700 to ~7000 years ago. When temporal distribution of 14C dated sequences from the Suceava black oaks were compared to the calibrated age ranges reported from nearby rivers (Siret, Moldova), deposition events were observed to coincide at around 0.8–0.9 ka cal BP and ~3.7–3.6 ka cal BP. The five presented floating chronologies, and especially the first 14C wiggle-matched tree-ring sequences of Ro-manian black oaks could become key building blocks in a longer regional oak tree-ring chronology for the Eastern Carpathian region.

Dendrochronological and radiocarbon analyses of subfossil oaks from the foothills of the Romanian Carpathians

Institute for Geological and Geochemical Research, MTA CSFK Lendület 2ka Palæoclimate Research Group, Budapest, Budaörsi  út 45, H-1112

National Research and Development Institute for Silviculture Marin Dracea, Silviculture Calea Bucovinei 73 bis, 725100, Câmpulung Moldovenesc,

Geochronometria

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

A set of subfossil macroremains, consisting of 118 oak (Quercus sp.) and 61 elm (Ulmus sp.) trees, was collected at five sites in the foothills of the Eastern...

Dendrochronological and radiocarbon analyses of subfossil oaks from the foothills of the Romanian Carpathians

Article Category: Research Article

Pubblicato online: 13 nov 2016

Pagine: 113 - 120

Ricevuto: 25 apr 2016

Accettato: 27 lug 2016

DOI: https://doi.org/10.1515/geochr-2015-0038

Parole chiave
black oak, Holocene, C-14, wiggle-matching, Suceava, Romania

© 2016 Z. Kern and I. Popa

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Dendrochronological and radiocarbon analyses of subfossil oaks from the foothills of the Romanian Carpathians

Article Category: Research Article

Pubblicato online: 13 nov 2016

Pagine: 113 - 120

Ricevuto: 25 apr 2016

Accettato: 27 lug 2016

DOI: https://doi.org/10.1515/geochr-2015-0038

Parole chiaveblack oak, Holocene, C-14, wiggle-matching, Suceava, Romania

© 2016 Z. Kern and I. Popa

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Parole chiave
black oak, Holocene, C-14, wiggle-matching, Suceava, Romania