Kaiser - Daettnau 3 Late Glacial Subfossil - PISY - ITRDB SWIT197 Kaiser, K. Kaiser, K. PISY Pinus sylvestris L. Scots pine Scotch pine earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3520; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3060; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3020; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3000; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3510; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (age,null,null,year Common Era,null,tree ring,null,null,N,null) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: DAEALCH3; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3540; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3500; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: KFKA3530; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999) earth science/paleoclimate/tree-ring (Daettnau 3 Late Glacial Subfossil>LATITUDE 47.4833>LONGITUDE 8.6833) Lateglacial and Holocene tree-ring chronologies are unique archives, which provide various information on past environments on a true annual time scale. Changes in ring-width can be related to past climate anomalies and dendrodated wood provides an ideal source for radiocarbon calibration. We present a 1051 year tree-ring chronology from the Late Glacial, built from subfossil Scots pines (Pinus sylvestris) that grew in different regions of Central and Southern Europe. Through a series of high-precision radiocarbon measurements we obtained a floating radiocarbon chronology, which allowed accurate wiggle-matching to the INTCAL98 calibration curve. The trees show a coherent pattern in ring-width variations throughout Central Europe, and extending into the Mediterranean, which indicates a strong external climatic factor, most probably temperature during the growing season. We identified major growth events, which appear synchronous with events seen in isotopic and tracer signals in the Greenland ice cores and with changes in the strength of upwelling in the Cariaco Basin. STUDY NOTES: Daettnau 3 Late Glacial Subfossil, Winterthur, Zurich, Switzerland # # Purpose of Collection: # Paeleoclimate, 14C calibration, extension of absolute tree-ring series # # Cores and cross-sections are stored at: # WSL Birmensdorf # # References: # Kaiser, K.F. (1993): # Beitrage zur Klimageschichte vom spaten Hochglazial # bis ins fruhe Holozan ... Ziegler Druck- und Verlags-AG, # Winterthur. 203p. # # Friedrich et al (2001): # High-resolution climate signals in the B?lling?Aller?d # Interstadial (Greenland Interstadial 1) as reflected in # European tree-ring chronologies compared to marine varves # and ice-core records. # Quaternary Science Reviews # Vol. 20, Issue 11, May 2001, pp. 1223-1232 # doi:10.1016/S0277-3791(00)00148-7 # # # Notes: # Subfossil wood, Late Alleroed, cal.BP 14,237 BP - 12,750 # Loam pit, substrate of UFM. Late Glacial timberline. # Daettnau (Alch3) # NOAA Template Raw Measurements file added 2019-02-05. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Kaiser, K. 2010-06-10 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/10723 https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/swit197.rwl https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/swit197-noaa.rwl https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/swit197.txt https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/swit197.rwl https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/swit197-noaa.rwl https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/swit197.txt English https://www.ncdc.noaa.gov/paleo/study/10723 https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/swit197.rwl https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/swit197-noaa.rwl https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/swit197.txt Friedrich, M., B. Kromer, K.F. Kaiser, M. Spurk, K.A. Hughen, and S.J. Johnsen. 2001. High-resolution climate signals in the Bølling-Allerød Interstadial (Greenland Interstadial 1) as reflected in European tree-ring chronologies compared to marine varves and ice-core records. Quaternary Science Reviews, Vol. 20, Issue 11, May 2001, pp. 1223-1232. doi:10.1016/S0277-3791(00)00148-7 START YEAR: 14237 cal yr BP * END YEAR: 12750 cal yr BP 8.6833 47.4833 8.6833 47.4833