Tree rings reveal dry conditions during Charlemagne's Fossa Carolina construction in 793 CE

0524039 - ÚVGZ 2021 RIV GB eng J - Článek v odborném periodiku
Muigg, B. - Seim, A. - Tegel, W. - Werther, L. - Herzig, F. - Schmidt, J. - Zielhofer, C. - Landa, A. - Büntgen, Ulf
Tree rings reveal dry conditions during Charlemagne's Fossa Carolina construction in 793 CE.
Quaternary Science Reviews. Roč. 227, JAN 2020 (2020), č. článku 106040. ISSN 0277-3791. E-ISSN 1873-457X
Grant CEP: GA MŠMT(CZ) EF16_019/0000797
Institucionální podpora: RVO:86652079
Klíčová slova: climate * precipitation * reconstruction * variability * extremes * region * dendroclimatology * temperature * regression * frequency * Bavaria * Carolingian period * Dendrochronology * Drought reconstruction * Early Middle Ages * Tree-rings * Paleoclimatology * Central Europe * Late Holocene * Anthropocene
Obor OECD: Physical geography
Impakt faktor: 4.112, rok: 2020
Způsob publikování: Open access
https://www.sciencedirect.com/science/article/pii/S0277379119308686?via%3Dihub

The first navigable canal across the main European watershed in southern Germany was the most ambitious and visionary hydro-engineering project of the Early Middle Ages, known as Charlemagne's Fossa Carolina. Hydrological conditions would have been crucial for both the construction process and subsequent navigability. Written sources specify that heavy rain was a crucial factor for the abandonment of the project in late 793 CE, a few months after digging began. Our understanding of past climate variability in this region is, however, limited by the lack of high-resolution proxy archives. Here, we use annually resolved and absolutely dated ring-width measurements of 2469 drought sensitive oaks (Quercus sp.) from Bavaria, Germany, to reconstruct regional changes in hydroclimate back to 500 CE. Periods of anomalously dry summers occurred from similar to 600 to 800, similar to 900-1000, similar to 1200-1400 and similar to 17001900 CE, whereas increased humidity characterized the 9th century, High Middle Ages (11th-12th century) and the 17th century CE. Relatively dry conditions during the construction period favoured the building progress of the Fossa Carolina. However, the heavy rain which stopped the project in 793 CE is not reflected in radial oak growth. This is likely related to i) the historically recorded event happened outside the growing season and ii) compared to dry extremes, wet extremes are generally less pronounced in tree-ring width. Nevertheless, our results provide the first local hydroclimate reconstruction covering the entire Early Middle Ages and thus, placing the Fossa Carolina in a long-term high-resolution environmental perspective. (C) 2019 Elsevier Ltd. All rights reserved.
Trvalý link: http://hdl.handle.net/11104/0308350