Mapping Ancient Africa: Video of seminar 19

July 26, 2024
WDG

On the 25 July 2024 the 19th Mapping Ancient Africa (MAA) seminar, entitled Climate frameworks for the Middle Stone Age and Later Stone Age in Northwest Africa, was delivered by Solène Boisard (University Montreal). In the seminar Solène presented two lines of evidence for past climate change in north-western Africa over the last c. 70,000 years. One from mechanistic climate models (via the PastClim package, for more details see: Leonardi et al. 2023) and one from reconstructions based on archaeological evidence. She found good agreement between the two approaches and linked climatic changes to the transition from Middle Stone Age to Late Stone Age technologies.

Details of this seminar can be found here. You can find more Mapping Ancient Africa seminar videos on the “Ecology of the Past” YouTube channel.

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Mapping Ancient Africa: Collaboration opportunity

July 26, 2024
WDG

COLLABORATION OPPORTUNITY: The TIP-TOP project, funded through the Dutch Research Council (NWO) and awarded to Rick Hennekam at the NIOZ Royal Netherlands Institute for Sea Research (NIOZ), is running from 2024-2029 and aims to use sediments accumulated in front of North African rivers to study environmental tipping points in North Africa. Specifically, the project focuses on available sediments from the Nile River delta, a now-dormant river system in Libya, as well as material from in front of the Senegal and Gambia rivers that will be acquired during a cruise early 2025. A multidisciplinary group of scientists is collaborating within this project, including scientists from NIOZ, GFZ Potsdam, ETH Zürich, Wageningen University, and the Utrecht University, using especially (in)organic and palynological proxies. Yet, we are keen to start new collaborations, especially with scientists based in northwest Africa. Potentially we could aim for the INQUA Fellowship Program For International Mobility (deadline 15 of September, 2024) for someone to gain international experience at one of the involved institutes for the duration of 3–6 months. If you are interested to link up with Rick please join the seminar to speak with him, or contact him directly. Note that participation in the 2025 expedition to the coasts of Gambia, Senegal, and Mauritania can be discussed too, but available places are very limited.

This video was recorded after the 19th online Mapping Ancient Africa seminar given by Solène Boisard, to watch her seminar on the past climate of north-western Africa and others in the series click here. To find out more about the Mapping Ancient Africa project click here.

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The long history of people in the rainforest of Suriname 

July 25, 2024
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In this article I summarize and describe the scientific research that was performed near Botopasi in Suriname, which was published in Ecology as ‘Pre-contact and post-colonial ecological legacies shape Surinamese rainforests’ (https://doi.org/10.1002/ecy.4272). 

Figure 1: Our research team in the field

Background

In October 2021, between COVID-19 restrictions, I joined archaeologist dr. Cheryl White and her team to excavate the remnants of a ‘lost village’ of Saamaka Maroons in the Surinamese rainforest. Maroons are the descendants of enslaved Africans, who, in the late 1600s, fled plantations to live in freedom in the Surinamese rainforests. Dr. White has been investigating the first villages and the movements of Suriname’s Maroon communities for decades and is an expert in this topic. 

Our wonderful research team consisted of Farisha Kartosemito B.Sc., Sushmeeta Ganesh B.Sc., Jõvan Samson B.Sc., Agir Axwijk B.Sc., Santosh Singh M.A., Thanya Fonkel MPA, Harrold Sijlbing, Dombi Lö, Gerno Eduards & Farik Eduards. We were welcomed in the village Botopasi, and after a day of hard work in the field, we enjoyed delicious Surinamese food and played troefcall!

As an ecologist, I was interested in the ecological effects of past human activities on the forest ecosystem. In these rainforests, Maroon and Indigenous communities often burn and remove trees near their homes to grow a variety of crops like cassava, tayer, maize and banana. After some years, the cultivation site is abandoned and forests can grow back. But do those forests recover back to their original state? 

What did the forest look like before people arrived and settled in the landscape of Boven Suriname?

To study how Maroon communities have shaped Surinamese forests over time, I made a reconstruction of the landscape of the past (going back thousands of years). The landscape was near an archaeological sites called ‘Beng Tau’, where Maroons lived in the 17th century. We used plant fossils and charcoal remains to reconstruct the forest from the past, to research if people were using fire and growing crops, and how the forests recovered from that.

Results and implications

Figure 2: Phytoliths from the banana plant

The charcoal remains and plant fossils, particularly from maize and banana, confirmed Saamaka Maroons settled in the area since ca. 1700 and practiced slash-and-burn agriculture was near the archaeological site called ‘Beng Tapu’ (Figure 2). The site may have been a cooking area, because remnants of pottery with maize, rice and banana were found. Within 1 km of Beng Tapu, we found large fragments of charcoal, and plant fossils from maize and banana. Smaller charcoal fragments and banana were found within 5 km of the archaeological site. Nowadays, agriculture is practiced within 8 km of the archaeological site and Suriname river. The area used for agriculture likely expanded over time. 

How did the forest recover from these activities? 

Within 1 km of the archaeological site, forests were burnt and used multiple times. Here, forests have a lower biomass than further away from Beng Tapu, meaning fewer or smaller trees have grown back. Also, Attalea and Oenocarpus palm trees increased. Still today, the Saamaka Maroon community uses the maripa palm to make oil. Therefore, the number of maripa palms may have increased due to human activities like cooking and oil production! Attalea and Oenocarpus palms are also adapted to open conditions and fire, showing the influence people had on the environment and how the forest responded to fires.

Further (2-7 km) away from the archaeological site, where disturbances were fewer, the forests recovered much better but Astrocaryum palms grew back in higher numbers in the understory of the forests. What makes these palms so resilient? We are still uncertain. The forests furthest away (>8km) from Beng Tapu showed little signs of disturbances. 

Figure 3: View from the Suriname River

A long human history, and an Indigenous archaeological site?

The Saamaka Maroons were not the first people to have inhabited the forests near Botopasi. Charcoal fragments show that people were in region (the ca. 20 km radius we studied) already 2000 years ago, and fire events occurred ca. 2000, 1700,1500, 1300, 1200 and 800 years ago. We don’t know which Indigenous Cultures may have inhabited this region, because of limited archaeological and historical research here. Large charcoal fragments were found ca. 7 km away from Beng Tapu, across the Suriname River. Could this be an Indigenous archaeological site?  

Conclusion

Our results show the timing, intensity and frequency of past disturbances are very important for good forest recovery and some disturbances from the past can still impact the modern vegetation. 

Unravelling the past not only tells us about the ancestors of Maroons and the lives of Indigenous communities before the 1500s. The past also helps us to understand how forests respond to human impacts. To better guide conservation strategies, we need to do more archaeological and ecological research in Surinamese rainforests. 

Next to the Suriname River, past human activities shaped the forest and increased local palm abundances. The broader forested region showed a healthy recovery. These results indicate that the Saamaka Maroon community preserved most of the forests they inhabited since the 1700s. We can learn from traditional knowledge about which management practices are sustainable to keep forests healthy. 

If you want to know more about the “hows” of this research… dive with me into the methodology! 

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Mapping Ancient Africa: Writing workshop videos

July 15, 2024
WDG

During the Mapping Ancient Africa (MAA) workshop in Kenya (3-6 June 2024) the session delivered by Rahab Kinyanjui (National Museums of Kenya) was recorded for those that could not make it. The seminar was focused on how to deal with reviewer comments. While this was targeted for participants focused on developing their manuscripts for the MAA special issue of Quaternary International (for full details click here). This seminar is relevant to all those facing reviewer comments on their scientific manuscripts.

Dealing with reviewer comments (Rahab Kinyanjui, National Museums of Kenya)

For further information on developing scientific manuscripts you might also be interested to check out our video on how to structure a scientific article (click here). For other MAA online content visit our YouTube channel for seminars, project updates, and to meet our scientists.

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Mapping Ancient Africa: Video of seminar 18

July 12, 2024
WDG

On the 20 June 2024 the 18th Mapping Ancient Africa (MAA) seminar was delivered by Kumar Akhilesh (Sharma Centre for Heritage Education). This seminar was a little different to most MAA seminars in that it focused on another INQUA project, rather than a specific research line. In the talk Kumar outlined the INQUA funded “PalaeoHome” project and highlighted work on hominin evolution in the Indian sub-continent.

Details of this seminar can be found here. You can find more Mapping Ancient Africa seminar videos on the “Ecology of the Past” YouTube channel.

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Mapping Ancient Africa: Seminar 19

July 11, 2024
WDG

The next Mapping Ancient Africa seminar will take place on 25 July 2024 at 17:00 CEST (15:00 GMT).

  • Speaker: Solène Boisard (University Montreal)
  • Title: Climate frameworks for the Middle Stone Age and Later Stone Age in Northwest Africa
  • Related publication: Boisard, S. & Arous, E.B. (2024) A critical inventory and associated chronology of the Middle Stone Age and Later Stone Age in Northwest Africa. Journal of Open Archaeology Data 12, 5. DOI: 10.5334/joad.121

The seminar will be delivered via Zoom. The link for the seminar can be obtained from the MAA Slack channel or by contacting the chair of this seminar (William Gosling). If you want to know more about the Mapping Ancient Africa project visit our web pages and please do not hesitate to get in contact if you want to get involved.

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MSc Earth Sciences: Peru field course 2024

July 10, 2024
WDG

The University of Amsterdam MSc Earth Sciences “Geoecological Systems” field course took place this year in Miraflores (Peruvian Andes) during June and July. Eighteen students, including three from Peruvian institutions, spent four weeks exploring the high Andes. During this time the students developed scientific projects to address interests of the local population related to soil quality, environmental pollution, water resources and cultural heritage. Access to the area and embedding within the community was enabled by The Mountain Institute Peru. During the course the students gained extensive ‘hands on’ field experience, developed teamworking skills and discovered the benefits of a participatory approach to research.

This course runs once every two years (to find out about the 2022 expedition click here). Want to join us on a future expedition? Check out our degree program here to enroll.

Images from the University of Amsterdam Peru field course 2024

Fire in Human Evolution

June 7, 2024
WDG

The “Fire in Human Evolution” international Symposium will take place at the University of Leiden (10-11 June 2024). The meeting is being organized by Femke Reidsma and Amanda Henry. The meeting will include talks and discussion on:

  • Fire perception, social interaction, and culture
  • Fire as landscape management
  • Fire, cooking and diet
  • Fire technology and cognition 
  • Archaeological signatures of fire

For full details click here.

SASQUA conference

June 6, 2024
WDG

South African research trip (part 1 of 3)

By Jelle Kraak

As part of my MSc Biological Sciences (University of Amsterdam) research project entitled “Assessing the effect of human induced fire regime changes on vegetation in the Drakensberg mountains” (for further details click to see previous post). I’ve travelled to Africa, where I’ll be staying a month. During this mini blogpost series I’ll take you with me on my travels! 

In the first week of my visit here, I along with my supervisor Prof. Trevor Hill and students from the University of Kwa-Zulu Natal went to visit the biennial SASQUA (Southern African Society for Quaternary Research) congress.

During the first poster session, I presented my poster which went into detail on how we are developing a proxy to reconstruct past fire using micro-Fourier Transformed Infrared Spectroscopy (µFTIR). These reconstructed fire temperatures can then be compared with phytolith or pollen data to assess the effects of different fire temperatures on local vegetation over time. The presentation and poster were well received!

After my poster presentation there were two more congress days which were filled with interesting talks and beautiful posters.

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Introducing: Jelle Kraak

June 5, 2024
WDG

Hello Ecology of the Past readers, my name is Jelle Kraak and I’m currently doing a research project for my MSc Biological Sciences (University of Amsterdam) supervised by William Gosling (University of Amsterdam), Jemma Finch (University of KwaZulu-Natal), and Trevor Hill (University of KwaZulu-Natal). The project is entitled: “Assessing the effect of human induced fire regime changes on vegetation in the Drakensberg mountains”. During the project I will visit South Africa to work at the University of KwaZulu-Natal and visit field site thanks to partial funding from the Amsterdam University Funds.

Research  project outline                                                                                 

As many of you know, humans have been interacting with the environment for millennia in various ways. One of the ways in which humans interact with the environment is through the ignition of fires. By doing so, humans may change fire regimes (fire frequency, severity and/or intensity), which in turn can cause changes in vegetation composition and structure. By using a combination of phytolith (local vegetation) and charcoal (fire) data from two sediment cores obtained from wetland environments in the Drakensberg mountains, we aim to assess the effect of fire regime changes on vegetation over the last 6000 years.

The phytoliths (biogenic silica microfossils) allow for the reconstruction of the past vegetation. Charcoal fragments characterize all aspects of past fire regimes: (i) frequency (time series analysis of charcoal data), (ii) severity (abundance of charcoal in samples reflecting biomass consumed), and (iii) intensity (spectral properties of individual charcoal fragments reflecting combustion temperature). 

The most interesting part of this project (in my humble opinion) is that this study is the first to use micro-Fourier Transformed Infrared Spectroscopy (µFTIR) to reconstruct fire temperatures from field samples ánd combine these accurately reconstructed temperatures with local vegetation data! It is important to accurately estimate fire temperatures, as the temperature of a fire dictates the type of plant materials which are consumed in a fire (the higher the temperature, the greater the proportion of woody material burning up). Similar studies have been conducted previously, however, these studies compared fire severity i.e. total burnt biomass with vegetation data. Although this works decently, total burnt biomass is not an accurate representation of fire intensity or temperature, as at very high temperatures biomass turns to ash, which cannot be detected in sediment cores. Through parameterizing both the vegetation changes and the fire regime we will provide a comprehensive picture of how changing human fire use practices modified the vegetation. We anticipate that: (i) a decrease in fire intensity resulted in woody encroachment of the surrounding vegetation, which was concomitant with the arrival of agropastoralists c. 600 years ago, and (ii) a shift in the proportion of C3 and C4 grass species in reaction to temperature changes in the Drakensberg mountains.

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