Neandertal

Excavaciones Arqueológicas en Pinilla del Valle (Comunidad de Madrid, España)

Excavaciones en Pinilla del ValleExcavaciones en Pinilla del Valle

El Museo Arqueológico Regional ha sido el impulsor de la creación de un nuevo equipo de investigación interdisciplinar para intervenir en los yacimientos del Calvero de la Higuera, en Pinilla del Valle (Madrid).

Descubierto en 1979 el primero de los yacimientos, la Cueva del Camino, fue excavado entre 1980 hasta 1989 por un equipo de la Universidad Complutense dirigido por F. Alférez. Desde 2002 viene siendo excavado por el equipo de investigación dirigido actualmente por Juan Luis Arsuaga (UCM-Carlos III), Enrique Baquedano (MAR) y Alfredo Pérez-González (UCM). Resultado de las primeras intervenciones es el descubrimiento de este enclave de gran interés paleontológico de unos 80.000 años de antiguedad. Además, entonces se descubrieron los dos primeros molares de Homo neanderthalensis. Fruto de los trabajos desarrollados por el equipo actual de investigación, es la constatación de que este yacimiento se trata de un cubil de hienas.

El Abrigo de Navalmaíllo, por su parte, fue descubierto en 2002. A diferencia de la Cueva del Camino, éste se trata de un campamento de neandertales. Fechado entre 70 y 77.000 años, conserva los restos de las actividades que grupos de homínidos realizaron aprovechando el abrigo de la roca. Aquí se conserva un interesante conjunto de industria lítica musteriense, principalmente realizada en cuarzo, que es el material más abundante en los alrededores, así como una rica asociación faunística producto del consumo de esos homínidos. Hay que destacar la preeminencia de especies de herbívoros sobre los carnívoros que están aquí escasamente representados.

La Cueva de la Buena Pinta, descubierta en 2003, al igual que ocurre con la Cueva del Camino fue usada como cubil de hienas durante el Pleistoceno. Estas introdujeron los restos faunísticos que muestran las marcas típicas de la actividad de carnívoros, así como abundantes coprolitos y restos de hienas inmaduras. Hay que destacar que durante la campaña de 2007 fueron localizados en el nivel 3 de la cueva dos molares de la especie Homo neanderthalensis pertenecientes al mismo individuo.

Por último, y en 2009, se descubrió otro complejo de galerías que se ha denominado Cueva Des-Cubierta. Al igual que ocurre con los tres anteriores, se trata de antiguas galerías rellenas por sedimentos fosilíferos. Aún está pendiente de datación y los restos de fauna e industria obtenidas aún son objeto de estudio. Sin embargo, lo más destacable de estos rellenos es la aparición en 2011 de varios restos dentales infantiles que, al igual que en los otros dos yacimientos, pertenecen a la especie Homo neanderthalensis.

Aproximadamente desde el 15 de agosto al 15 de septiembre de cada año se llevan a cabo excavaciones de verano en los yacimientos del Calvero de la Higuera. Estos días estamos preparando ya la próxima campaña y puedes ver este video de Javier Trueba sobre las excavaciones de 2011.

Copyright © Museo Arqueológico Regional de la Comunidad de Madrid

Tracing Neandertal Territories in the Mountains of Southeast France

Day of Archaeology 2013 for me means being away on 2 months of fieldwork in the southern Massif Central, France.  I’ve been contributing to DOA since 2011, and if you look back, it’s clear a lot has changed  since then (see my four 2011 posts, and 2012). After my PhD I was searching for a postdoc for several years, ran out of time and money to keep looking, and ended up seredipitously with a contract to write a book about humans and birds in prehistory.

I thought that would be it, and that the 2013 Day of Archaeology would take place without a contribution from me. But it seems that archaeology wasn’t quite done with me…

My workspace at the field station, Laussonne, Haut Loire

My workspace at the field station, Laussonne, Haut Loire

As I wrote in a postscript comment to my post last year, only a few days after writing about the difficult process of changing paths from a research career to one focused on writing and wider communication, an email dropped into my inbox from the European Commission offering the very last postdoc funding I applied for- a Marie Curie Intra European Fellowship to work in at the PACEA lab, Universite of Bordeaux. After a lot of soul-searching on the wisdom of doing another 180 degree turn in my life trajectory, and talking with my husband about him coming out with me, I decided to go for it. And so here I am, in the mountains of the Massif Central!

Laussonne map

Laussonne map

The field station for Archeo-Logis at Laussonne, Haut Loire

The field station for Archeo-Logis at Laussonne, Haut Loire

My postdoc is focused on two elements: training in a new skill (the Marie Curie Fellowships are especially concerned with career development), and applying this method to an archaeological context. I’ve written on my own blog in more detail about my project, which is called TRACETERRE. This stands for “Tracing Neandertal Territories: Landscape Organisation and Stone Resource Management“. It’s part of a larger collaborative project directed by my boss, Jean-Paul Raynal, and Marie-Helene Moncel.

Essentially I’ll be learning a detailed geological technique called petro-archaeology, that allows us to determine where in the landscape Neandertals were obtaining the raw materials to make their stone tools. Specifically, we are especially interested in the flint sources: most of the geology in the area is igneous, which means it comes from volcanic action (the Massif Central is a world famous centre for volcanology, where you can see virtually every type of volcano and lava).

Sancy Massif

Sancy Massif, north of where I am based, showing volcanic formations

It’s possible to make stone tools from these kinds of rocks, but they are often very hard, and can also be coarse. Flint is a sedimentary rock, meaning it forms from the slow accumulation of mineral deposits. Flint is famous for the high quality tools that can be made from it, because of the predictable way it fractures. It’s often associated with Cretaceous chalk deposits, such as the big cliffs in the southern UK, where you can see black bands of flint nodules. So flint forms in marine contexts, but it can also form in other situations such as in lakes.
Although there are few primary sources of flint in the Massif Central (i.e. outcrops of rock containing flint), there are many different secondary sources. These can be eroded outcrops, material washed into river gravels and other kinds of sources. My training will be in identifying these secondary types of sources, based on the way the outer surface of flint cobbles changes during the process of first formation, erosion and later exposure at archaeological sites.

Some of the geological reading I've been getting up to speed on. Volcanoes galore!

Some of the geological reading I’ve been getting up to speed on. Volcanoes galore!

Because there are more than 70 different secondary sources in the region which have been painstakingly identified over more than thirty years (by Paul Fernandes, who will train me), this is too much to try to attempt to learn in two years. So I will be using a source-centred approach, where I look at one flint source, and see how this particular rock has been used by Neandertals. In particular, we are interested in where this rock ends up: which caves or open-air archaeological sites is it found in? And secondly, in what form does it occur: as finished tools, raw blocks, or flakes of stone that have been struck off blocks (cores) but not yet made into tools.

Finding these things out can tell us a huge amount about techno-economics: the way in which Neandertals were choosing to organise their exploitation of resources on landscape scales. For example, working out which types of technology they used to make tools and which stages of tool production occur where can reveal the level of investment of energy: were they making tools quickly, and dropping them soon afterwards? Or were they carefully choosing which kinds of tools to make, and which ones to take with them in toolkits, maintaining them by re-sharpening? Both these strategies can be used as adaptations to different situations, particularly the level of mobility.

A handaxe, one type of tool Neandertals seem to have carried with them as part of mobile toolkits, which could be re-sharpened and used in many tasks. This one is from near Bournemouth, UK

A handaxe, one type of tool Neandertals seem to have carried with them as part of mobile toolkits, which could be re-sharpened and used in many tasks. This one is from near Bournemouth, UK

The question of Neandertal mobility is also a key reason for studying in such detail the different sources of stone used. We want to know where the stone from a flint source was going: which sites is it found in? How far was flint being transported, especially in comparison to other stone types? We can even begin to work out the paths taken through the landscape by Neandertals: did they have to cross rivers, high mountainous areas? Which passes would have been likely to be used? We also plan to excavate at the flint source itself, to see what activities were taking place, and also which tools came from other places in the landscape.

We can then begin, by combining all the geological and techno-economic data, to build up a detailed understanding of the inter-connections between different parts of the landscape that Neandertals were living in. And this is just the stone tools: other parts of the archaeological record, such as animal bones preserved in caves, are studied by other project members. We can use these to determine things like what season people were living at sites, and where they were probably hunting the animals in the landscape.

Gravel bar system, Switzerland- one example of a secondary source of stone. Image used with permission via Creative Commons: " I, Paebi [GFDL (http://www.gnu.org/copyleft/fdl.html), CC-BY-SA-3.0 (http://creativecommons.org/licenses/by-sa/3.0/) or CC-BY-SA-2.5-2.0-1.0 (http://creativecommons.org/licenses/by-sa/2.5-2.0-1.0)], via Wikimedia Commons"

Gravel bar system, Switzerland- one example of a secondary source of stone. Image used with permission via Creative Commons: ” I, Paebi CC-BY-SA-2.5-2.0-1.0 (http://creativecommons.org/licenses/by-sa/2.5-2.0-1.0)], via Wikimedia Commons”

All this creates a web of the palaeo-landscapes that Neandertals were inhabiting. But the impact of sourcing flint tools goes even further, because if we can map the extent of inhabited landscapes, we can start to think about territories. This is crucial because territories are not just regions full of resources- they probably were also involved in defining social interactions between different Neandertal groups. This is something we are still learning how to measure, but it has huge significance because different kinds of territories and social interactions suggests particular cognitive capacities. This is of course one of the key areas of research in human evolution: how did Neandertals differ from us, and how were they similar? Did they have similar webs of social connections, or were they living local, isolated lives in small groups that did not regularly meet? If this was the case, how did they find mates, and prevent huge in-breeding? All these fundamental questions can be advanced by new data and investigations such as the research I am doing.

Right now, I’ve only been here just over a week, and am only one month into a two year postdoc. So there’s a long way left to go. But it’s very exciting, and I hope to start the petro-archaeology training and looking at the flint collections very soon. Meanwhile, there’s always time on fieldwork to have a day off, check out the local wildlife, cuisine and culture, and enjoy some of the lovely sunsets in this region. Very different landscapes to when Neandertals were living here!

 Sunset at Laussonne

Sunset at Laussonne

I am funded through a European Commission Framework 7 Marie Curie Intra-European Fellowship for Career Development, and I work at the PACEA laboratory, UMR-5199, Universite Bordeaux 1.

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