Henri-Georges Naton
Géoarchéon, Géoarchéologie, Faculty Member
ABSTRACT Tufa deposits are proven to record high quality palaeoenvironmental and palaeoclimatic information. They also appear to be influenced by human activities as indicated by the ‘late Holocene tufa decline’ observed in Europe from... more
ABSTRACT Tufa deposits are proven to record high quality palaeoenvironmental and palaeoclimatic information. They also appear to be influenced by human activities as indicated by the ‘late Holocene tufa decline’ observed in Europe from the Atlantic optimum, when tufa should be well developed regarding climatic conditions. The studied tufa comes from the Mamer Valley in Luxembourg: Direndall. As it covers a broad part of the Holocene, this deposit offered a great opportunity to discuss modalities and timing of the tufa decline and the human impact on fluvial formations since the early Holocene. Recent fieldwork at Direndall allowed the collection of new stratigraphic data and samples for a geochemical study. We investigate calcite stable isotopes as records of past temperature and humidity conditions. Comparisons with the environmental reconstructions from a previous malacological study show strong consistency with the δ13C record and suggest humidity might have been the main factor controlling environment evolution at Direndall. Despite the climatic variations observed, none explains the environmental change towards open conditions while optimum forest develops as recorded by molluscs at the top of the sequence. This episode is likely to be linked to local anthropogenic forest clearance during the Roman occupation. However, no clear impact of human activity has been observed in the tufa stratigraphy or precipitation rate. The exceptionally long Direndall tufa sequence thus provided outstanding palaeoenvironmental and palaeoclimatic data and might become, together with the underlying fluvial and colluvial deposits, a reference site for the Holocene and Tardiglacial in Luxembourg and surrounding areas.
Research Interests:
A new multidisciplinary study is in progress at Direndall in the Mamer Valley in Luxembourg, combining stratigraphy, geochemistry, malacology and palynology. As it covers a wide part of the Holocene (C14 dating between c. 10 000 to 900 ka... more
A new multidisciplinary study is in progress at Direndall in the Mamer Valley in Luxembourg, combining stratigraphy, geochemistry, malacology and palynology. As it covers a wide part of the Holocene (C14 dating between c. 10 000 to 900 ka BP), the 8m-high tufa deposit provides a great opportunity to discuss modalities and timing of the so-called ‘late Holocene tufa decline’ (Goudies et al., 1993) and the combined controls of climate and human activity on fluvial formations since the Early Holocene. Recent fieldworks at Direndall allowed collection of new stratigraphical data and samples for a geochemical study. We investigate calcite stable isotopes (δ18O and δ13C) and Mg/Ca and Sr/Ca ratios from Direndall tufa as records of past temperature and humidity conditions. Comparisons with the environmental reconstructions from a previous malacological study (Meyrick, 2000) show strong consistency with the δ13C record suggesting that humidity might have been the main climatic factor contro...
The Alzette River rises within France, approximately 4 km south of the French-Luxembourg border, and has a total length of 73 kilometres before joining the Sauer which is a left-bank tributary of the Moselle River. During the construction... more
The Alzette River rises within France, approximately 4 km south of the French-Luxembourg border, and has a total length of 73 kilometres before joining the Sauer which is a left-bank tributary of the Moselle River. During the construction of the" Nordstrooss" ...
Research Interests:
... Pierre BINTZ*, Jean-Jacques DELANNOY**, Henri-Georges NATON***, Marc CARTONNET**** & Thierry TILLET*****. ... 2. les dépôts riches en éléments grossiers issus de la géliva-tion des calcaires des parois avoisinantes se mettent... more
... Pierre BINTZ*, Jean-Jacques DELANNOY**, Henri-Georges NATON***, Marc CARTONNET**** & Thierry TILLET*****. ... 2. les dépôts riches en éléments grossiers issus de la géliva-tion des calcaires des parois avoisinantes se mettent en place à partir du Tardiglaciaire. ...
