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Madagascar copal: New dating for an Antropocene ancient resin

The study states that the well-known Madagascar copal is not a semi-fossilized resin but a material made during the Antropocene. This ancient resin which was not completely fossilized comes from Hymenaea verrucosa trees. The study notes that any new described taxon after the Madagascar copal should be attached the dating of Carbon for the studied sample.

The known Madagascar copal is a more recent resin from what was thought -it has about a few hundred years- and trapped pieces in this material are not as palaeontological important as thought traditionally. The study states that the well-known Madagascar copal is not a semi-fossilized resin but a material made during the Antropocene, historical period in which human impact was extreme globally.

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Madagascar copal: new dating for an Antropocene ancient resin

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On June 7, in the English city of Bristol, protesters removed a statue of the local slave trader Edward Colston. In the days that followed, Please enable JavaScript! Bitte aktiviere JavaScript! Por favor,activa el JavaScript! The known Madagascar copal is a more recent resin from what was thought -it has about a few hundred years- and trapped pieces in this material are not as palaeontological important as thought traditionally.

Recent resin formation on Hymenaea trees in Madagascar [Credit: Xavier Delclos] The study states that the well-known Madagascar copal is not a semi-fossilized resin but a material made during the Antropocene, historical period in which human impact was extreme globally. The findings would require going over the described taxon during the last hundred and fifty years to avoid taxonomic mistakes and unprecise paleoenvironmental reconstructions, the study notes.

Known for hundreds of years, the Madagascar copal crossed the trade routes from Tanzania to China through the Indian Ocean and the Indian markets. Sold as incense at first, it became pricey due to its high value to make varnish.

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Madagascar copal: New dating for an Antropocene ancient resin. This material is not a semi-fossilized resin. University of Barcelona.

We present an overview on different environmental zones within coastal areas and summarise the physical basis behind the three most important methods that are available to date Holocene coastal sediments. Besides radiocarbon and uranium series dating, Optically Stimulated Luminescence O sl has increasingly been applied for dating in coastal settings over the past decade. This is illustrated by a number of case studies showing that O sl can be applied to sediments from almost any kind of coastal environment, covering a potential dating range from some years up to several hundred thousand years.

O sl dating may hence be the method of choice for deciphering natural environmental change along coasts as well as the presence and the impact of human occupation in such areas. In addition, we briefly show how and where these dating methods could be applied to constrain the palaeo-environmental context of an archaeological site at Vohemar in north-eastern Madagascar.

Comments from Tony Reimann on an earlier version are greatly appreciated. From the geological perspective, coasts are highly dynamic areas with short frequency but low amplitude changes caused by daily low and high tides, and occasional storm events partially having a high impact on geomorphology. Long term trends are due to raising or decreasing sea level caused by global climate change, and emerging or sinking coast lines due to tectonic movements.

Climate change also affects the frequency and magnitude of severe storm events e. Additionally, seismic events, often occurring thousands of kilometres away, may cause substantial modification of coastal areas. This was recently dramatically demonstrated by the devastating tsunamis in the Indian Ocean in and off the eastern coast of Japan in Examples are available from the southern Baltic Sea e. Schwarzer et al. The problem is that these approaches only cover the last few centuries and that not all regions have been mapped in detail in the historic past.

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The Madagascar results are equally intriguing since they are from two regions on the island. These basalts (and gabbros) are thought by conventional geologists.

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Symposium on Geol. Resources of Madagascar – A good example of the usefulness of the in-situ dating method. Madagascar displays a huge portion of the lower crust and its study is fundamental for the understanding of the evolution of this part of the crust. Unfortunately, our knowledge of this domain is limited. At this time, numerous works structural, geochemical, petrological are in progress in Madagascar, but there are only a few geochronological data.

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The known Madagascar copal is a more recent resin from what was thought -it has about a few hundred years- and trapped pieces in this material are not as palaeontological important as thought traditionally. The study states that the well-known Madagascar copal is not a semi-fossilized resin but a material made during the Antropocene, historical period in which human impact was extreme globally.

The findings would require going over the described taxon during the last hundred and fifty years to avoid taxonomic mistakes and unprecise paleoenvironmental reconstructions, the study notes. Known for hundreds of years, the Madagascar copal crossed the trade routes from Tanzania to China through the Indian Ocean and the Indian markets.

Sold as incense at first, it became pricey due to its high value to make varnish. More recently, it was used as disinfectant -burnt in Madagascar houses- and it was sold to scientists and tourists for its high content of arthropods inside. This ancient resin which was not completely fossilized comes from Hymenaea verrucosa trees, a fabacean that grows in the eastern coast of Madagascar, one of the most threatened and fragile ecosystems in the world.

According to the study, the scientific community studied the biological remains inside the copal, named bioinclusions, and dated these findings from a few tens to millions of years. However, the origin of the studied material was never found -it is not cited in any study-, and the exact age of the studied pieces was never proved. According to the study, some found species in the Madagascar copal -thought to be extinct- could be now in forest habitats that were not considered to be their natural habitats.

This can explain the occasional presence of arthropod species inside this old resin and which are currently living in the area. The study notes that any new described taxon after the Madagascar copal should be attached the dating of Carbon for the studied sample at least, the sample including the main piece or holotype.

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