Support the collection of subfossil wood of glacial origin throughout the Alps (France, Switzerland, Italy, Austria) in order to date Holocene glacial variations very precisely using dendrochronology!

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The «all or nothing» principle applies: The project only receives the funds if the funding target is reached or exceeded.

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Sampling campaign for subfossil wood of glacial origin in the Alps

Help me collect the latest subfossil glacial woods!

As we are seeing today with glacial collapse around the world, glaciers are the most visible indicators of climate change. Less well known, trees can tell similar stories, with even finer temporal resolution (annual)!

The intersection of the two constitutes a unique field of research called ’dendroglaciology,’ which studies periods when glacier fronts interacted with forests in the past. It is interesting to note that dendroglaciology shares much with ’preventive archaeology’ in terms of working under urgent conditions!

This project goes far beyond the academic world and aims to build up a sufficiently large corpus of wood to be used in the future for analyses that we do not yet know how to carry out. Subfossil wood allows us to reconstruct pre-industrial temperatures with unparalleled resolution. Our work is therefore in line with projects such as ICE MEMORY, in which glaciologists recover ice cores to preserve and study them in the future, when the glaciers have disappeared!

  • Mer de Glace - tree date: 1120 CE
    Mer de Glace - tree date: 1120 CE
  • Sampling beneath the ice!
    Sampling beneath the ice!
  • Aletsch - Bronze age fossil soil (date: 1500 BCE)
    Aletsch - Bronze age fossil soil (date: 1500 BCE)
  • Mer de Glace - late roman period maple tree (date: 312 CE)
    Mer de Glace - late roman period maple tree (date: 312 CE)
  • Mer de Glace - late Roman Period maple tree (date; 312 CE)
    Mer de Glace - late Roman Period maple tree (date; 312 CE)
  • Tschierva Glacier forefield
    Tschierva Glacier forefield
  • 10,000 year old pristine bark!
    10,000 year old pristine bark!
  • Morteratsch - Perfect cookie!
    Morteratsch - Perfect cookie!
  • Mer de Glace - One of the largest trunk ever sampled (date: 600 BCE)
    Mer de Glace - One of the largest trunk ever sampled (date: 600 BCE)
  • Arolla - in situ stump sheared by advancing glacier during the Little Ice Age
    Arolla - in situ stump sheared by advancing glacier during the Little Ice Age
  • Mer de Glace - examining sample
    Mer de Glace - examining sample
  • Morteratsch - relieved to have sampled one of most beautiful sample ever! date: 1317 CE
    Morteratsch - relieved to have sampled one of most beautiful sample ever! date: 1317 CE
  • Bossons - Large spruce trunk dated to 270 CE
    Bossons - Large spruce trunk dated to 270 CE
  • Mer de Glace - beautiful in situ stump in the lateral moraine dated to 1000 BCE
    Mer de Glace - beautiful in situ stump in the lateral moraine dated to 1000 BCE
  • Bringing back samples and gear always involves heavy lifting (20-40kg)!
    Bringing back samples and gear always involves heavy lifting (20-40kg)!

My project is unique because we are the only team in the Alps capable of collecting and accurately dating these unique pieces of evidence of past climates, which are very ephemeral and will no longer be found in the future.

Recovering these samples – which constitute a formidable archive of the past – can only be done during a short period of the year (at the end of summer) and, above all, during a fairly short period of ’deglaciation’ (a few decades)!

Then, it is TOO LATE!

These glacial subfossil trees began to be discovered in the 1970s, but it is only since the 2000s that they have been the subject of more in-depth studies. Unfortunately, this window of opportunity for their discovery will soon close, as we approach the Holocene glacial minimum. Due to the rapid evolution of proglacial margins under the effect of global warming, moraines are disappearing and stabilising at an increasingly rapid rate. In this context, missing a year of sampling means that all samples appearing that season in areas that are still ’geomorphologically active’ will be lost forever, as they will quickly be exported downstream and buried by alluvial or slope deposits.

I have been doing this work in the Alps for 16 years. Most of the time (9 of those 16 years), I have funded the annual field inspections with my own funds, mainly because they were not part of any ongoing project (or because I was not employed in research).

This is what we call passion and dedication.

But this year, I don’t have the funds necessary to carry out the sampling season.

These pieces of wood are our fragile heritage.

With your help, I will be able to make these last witnesses of past climates speak!

  • Bossons - spruce sample dated to 253 CE
    Bossons - spruce sample dated to 253 CE
  • Gorner - larch tree killed by an advance 8,200 year ago!
    Gorner - larch tree killed by an advance 8,200 year ago!
  • Morteratsch - larch tree killed by an advance 10,350 yr ago!
    Morteratsch - larch tree killed by an advance 10,350 yr ago!
  • Aletsch - Beatiful larch tree killed by the glacier around 620 CE
    Aletsch - Beatiful larch tree killed by the glacier around 620 CE
  • Aletsch - close up of a larch tree  highlighting the rings following the 536 CE volcanic eruption
    Aletsch - close up of a larch tree highlighting the rings following the 536 CE volcanic eruption
  • Typical glacier subfossil stone pine
    Typical glacier subfossil stone pine
  • Sanding machine setup
    Sanding machine setup
  • Sanding a large cookie!
    Sanding a large cookie!
  • The joys of sanding!
    The joys of sanding!

This is what I need backing for.

Concretely, the money will be used for :

  • 20 days fieldwork session in the Alps : travel, accomodation, chainsaw gear.
  • Radiocarbon dating of 10 wood samples (not datable by dendrochronology).
  • Preparation of proposed counter-proposals for this project (photographs, wood samples).
  • The use of the money will be explained and the account/results of the fieldwork will be published this autumn.
  • Tree ring measurement setup
    Tree ring measurement setup
  • Close up of tree ring measurement setup with a large cookie
    Close up of tree ring measurement setup with a large cookie
  • Close up of tree ring measurement setup. Razor blades are used to surface the wood.
    Close up of tree ring measurement setup. Razor blades are used to surface the wood.
  • Mont Blanc massif chronology synchronised with the Eastern Alpine Chronology over Medieval Period
    Mont Blanc massif chronology synchronised with the Eastern Alpine Chronology over Medieval Period
  • Oldest sample found at Mer de Glace synchronized with the Eastern Alpine Chronology (date: 2727 BCE)
    Oldest sample found at Mer de Glace synchronized with the Eastern Alpine Chronology (date: 2727 BCE)
  • Stone pine wood anatomy highlighting damage to the early 1171 CE cells caused by frost following a volcanic eruption
    Stone pine wood anatomy highlighting damage to the early 1171 CE cells caused by frost following a volcanic eruption
  • Subfossil wood storage facility at Savoie Mont Blanc University (Chambéry)
    Subfossil wood storage facility at Savoie Mont Blanc University (Chambéry)