Cited by 298Tree-ring climate responsesArchaeology and ancient environmental studiesGeology and Paleoclimatology Research

The DOI matches its Crossref record; 12 of the 12 references it cites were found in a registry or an index.

The 12,460-Year Hohenheim Oak and Pine Tree-Ring Chronology from Central Europe—A Unique Annual Record for Radiocarbon Calibration and Paleoenvironment Reconstructions

Open access

Abstract

The combined oak and pine tree-ring chronologies of Hohenheim University are the backbone of the Holocene radiocarbon calibration for central Europe. Here, we present the revised Holocene oak chronology (HOC) and the Preboreal pine chronology (PPC) with respect to revisions, critical links, and extensions. Since 1998, the HOC has been strengthened by new trees starting at 10,429 BP (8480 BC). Oaks affected by cockchafer have been identified and discarded from the chronology. The formerly floating PPC has been cross-matched dendrochronologically to the absolutely dated oak chronology, which revealed a difference of only 8 yr to the published 14 C wiggle-match position used for IntCal98. The 2 parts of the PPC, which were linked tentatively at 11,250 BP, have been revised and strengthened by new trees, which enabled us to link both parts of the PPC dendrochronologically. Including the 8-yr shift of the oak-pine link, the older part of the PPC (pre-11,250 BP) needs to be shifted 70 yr to older ages with respect to the published data (Spurk 1998). The southern German part of the PPC now covers 2103 yr from 11,993–9891 BP (10,044–7942 BC). In addition, the PPC was extended significantly by new pine chronologies from other regions. A pine chronology from Avenches and Zürich, Switzerland, and another from the Younger Dryas forest of Cottbus, eastern Germany, could be crossdated and dendrochronologically matched to the PPC. The absolutely dated tree-ring chronology now extends back to 12,410 cal BP (10,461 BC). Therefore, the tree-ring-based 14 C calibration now reaches back into the Central Younger Dryas. With respect to the Younger Dryas-Preboreal transition identified in the ring width of our pines at 11,590 BP, the absolute tree-ring chronology now covers the entire Holocene and 820 yr of the Younger Dryas.

Overview

The claims and statistics of this paper haven’t been checked yet.

Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.

A few free checks a day · papers already verified open instantly · results are public

Integrity signals

Registry

Crossref · 10.1017/s003382220003304x

Cites

12 of 12 references verified0 citation errors · 0 not checkable

Statistics

Verification

Claims the paper makes

The claims and statistics of this paper haven’t been checked yet.

Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.

A few free checks a day · papers already verified open instantly · results are public

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • A major inter-comparison exercise using late glacial floating kauri tree-ring sequences resulted in a 14C wiggle-match, with correction for interhemispheric offset, to the European Preboreal Pine (PPC) chronology.

    “Amajor inter-comparison exercise using late glacial floating kauri tree-ring sequences (Hogg et al. 2016) resulted in a 14 Cwiggle-match, with correction for the interhemispheric offset, to the European Preboreal Pine (PPC) chronology (Friedrich et al. 2004).”

    From The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP) (2020) · cites this paper as Friedrich et al. 2004

Self-check

Percentages, sums and reported differences re-computed from the paper’s own numbers.

The self-check needs the paper’s full text.

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 8

  1. Leuschner, 1992, Tree Rings and Environment. Proceedings of the International Dendrochronological Symposium, Ystad, South Sweden, 3–9 September 1990.
  2. Becker, 1983, Postglaziale Auwaldentwicklung im mittleren und oberen Maintal anhand dendrochronol-ogischer Untersuchungen subfossiler Baumstammablagerungen, Geologisches Jahrbuch, A 71, 45
  3. Becker, 1985, Dendrochronologie in der Ur- und Frühgeschichte., 8
  4. Becker, 1982, Dendrochronologie und Paläoökologie subfossiler Baumstämme aus Flussablagerungen. Ein Beitrag zur nacheiszeitlichen Auenentwicklung im südlichen Mitteleuropa, Mitteilungen der Kommission für Quartärforschung der Österreichischen Akademie der Wissenschaften., 5
  5. Strasser, 1999, Sédimentation postglaciaire fluviatile et palustre près d'Avenches (Suisse): implications climatique, Bulletin de la Societé Fribourgeoise des Sciences Nataturelles, 88, 5
  6. Kaiser KF . 1993. Beiträge zur Klimageschichte vom Hochglazial bis ins frühe Holozän, rekonstruiert mit Jahrringen und Molluskenschalen aus verschiedenen Vereisungsgebieten [Habilitation thesis]. Winterthur, Birmensdorf: Ziegler Druck- und Verlags-AG.
  7. Hurni, 1999, Exploitation dendrochronologique et analyses 14C, Mémoires de la Société Vaudoise des Sciences Naturelles, 19
  8. Spurk, 1999, Dendrochronologische, palynologische und Radiokarbon-Untersuchungen eines Waldes aus der Jüngeren Tundrenzeit. Naturwissenschaftliche Untersuchungen zum Weichselspätglazial in der Niederlausitz bei Cottbus (Land Brandenburg), Quartär, 49/50

Cited by

Sorted by citations

Metadata

Authors
Friedrich, M., Remmele, S., Kromer, B., Hofmann, J., Spurk, M., Felix Kaiser, K., Orcel, C., & Küppers, M.
Affiliations
  • University of Hohenheim (DE)
  • Heidelberg Academy of Sciences and Humanities (DE)
  • Laboratoire Romand de Dendrochronologie (CH)
Venue
Radiocarbon
Published
2004
Volume
46
Issue
3
Pages
1111-1122
ISSN
  • 0033-8222 (ISSN-L)
  • 1945-5755
OpenAlex
W1942153202
Cited by
298
References
12
Citations by year
2026: 6 · 2025: 5 · 2024: 12 · 2023: 13 · 2022: 10 · 2021: 13 · 2020: 21 · 2019: 15 · 2018: 15 · 2017: 17 · 2016: 18 · 2015: 9 · 2014: 27 · 2013: 13 · 2012: 18
FWCI
6.10
Type
journal article
Language
en
Open access
Locations
  • Radiocarbon (publishedVersion)
  • UA Campus Repository (The University of Arizona) (acceptedVersion)
  • DORA WSL (Swiss Federal Institute for Forest, Snow and Landscape Research) (submittedVersion)
Funders
Bundesministerium für Bildung und Forschung
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tree-ring climate responses
  • Social Sciences › Archeology › Archaeology and ancient environmental studies
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Keywords
tree-ring chronology, Holocene, Younger Dryas, Preboreal, radiocarbon calibration, Central Europe, paleoenvironmental reconstruction

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review