Visit at Umbeli Beli rock shelter

In March 2020, I had the opportunity to visit Umbeli Beli, a rock shelter located in KwaZulu Natal, South Africa with archaeological deposits spanning from the Middle Stone Age, until today.  The site is excavated by a team from Tuebingen University lead by Nicholas Conard and Gregor Bader.

Umbeli Beli Excavation 2020
Umbeli Beli 2020 excavation season

I am very fortunate to be involved in the study of the stratigraphy and Site Formation Processes in Umbeli Beli. Working together with Chris Miller, I will be looking at micromorphological thin sections of the site. The purpose of my latest site visit was to inspect the stratigraphy macroscopically and to acquire some more micromorphological samples. In addition, I had the chance to see archaeological finds from the excavation and become familiar with the raw materials.

Umbeli Beli micromorphology sampling
Conducting micromorphology sampling at Umbeli Beli using plaster

Umbeli Beli is located within close proximity to Umhlatuzana, they are both developed on similar lithologies (Natal Sandstones/Quartzites), and they occupy a similar archaeological time span (Middle Stone Age, Later Stone Age, Iron Age). A comparison between the two sites, both from a geoarchaeological and archaeological perspective, will be very interesting and informative!

Though short, my Umbeli Beli visit was amazing and full of awesome memories. Hopefully, I will be able to visit or work with the excavation team again in the future.

Kwazulu Natal beach
Beautiful beach in front of the excavation house

 

 

 

More info on the Umbeli Beli research:

Bader, G.D., Cable, C., Lentfer, C., Conard, N.J. (2016). Umbeli Belli Rock Shelter, a forgotten piece from the puzzle of the Middle Stone Age in KwaZulu-Natal, South Africa. Journal of Archaeological Science: Reports, 9, 608-622.

Bader, G.D., Tribolo, C., Conard, N.J. (2018). A return to Umbeli Belli: New insights of recent excavations and implications for the final MSA of eastern South Africa. Journal of Archaeological Science: Reports, 21, 733-757.

 

 

 

Thoughts on stratigraphy and sampling

I came across a paper by Tipper (1998) which reminded me of the importance of looking at stratigraphy in multiple dimensions. In the paper he discusses stratigraphic completeness and the notion of ‘‘spatio-temporal masking’’: the effect when primarily spatial variations mask primarily temporal variations. He then tries to estimate the optimum sizes of the sampling area in order to best estimate the stratigraphic completeness in the field. Admittedly, I did not follow Tipper’s calculations at some parts but two things became clear to me: the problems that this paper discusses are very relevant to specifically micromorphology and micromorphological sampling, and that it is very important to have micromorphology samples of at least two orientations when studying a site. 

Unfortunately, at Umhlatuzana it was only possible to sample the west profile. To solve the problem of having only N-S oriented samples, I ended up cutting some of the thicker samples vertically after impregnation. So, even if they were originally sampled at the west profile, they ended up having an E-W orientation.

The term spatio-temporal masking discussed by Tipper reminded me of the Law of Facies (aka Walther’s Law), a stratigraphic term explaining how depositional environments that are laterally related can become superimposed and result in trans-transgressive sedimentary formations (see more at Karkanans and Goldberg 2018, 163). The Law of Facies is for me one of the most complicated stratigraphic principles to fully comprehend but something you always have to take into account when studying a stratigraphic sequence.

Karkanas, P., & Goldberg, P. (2018). Reconstructing archaeological sites: Understanding the geoarchaeological matrix. Hoboken, NJ: John Wiley & Sons.

Tipper, J.C. (1998). The influence of field sampling area on estimates of stratigraphic completeness. Journal of Geology, 106(6), 727-738.

Recap of 2019

2019 has been relatively productive for my PhD research. Here I am going to overview some of the activities undertaken and their various ups and downs! 

Conferences attended

With participation in three international conferences (happening within a small time period), I would say that 2019 was rather conference heavy! 

In June I attended the Developing International Geoarchaeology conference in Vancouver, Canada. There I presented a poster and got to meet many interesting researchers in geoarchaeology, including the conference organizer Francesco Berna and his team. Link for poster.

In July I attended the Association of South African Professional Archaeologists conference in Kimberley, South Africa. It was a very nice experience that gave me the opportunity to meet many archaeologists that work or study in South Africa. Link for poster.

Lastly, in September I attended the European Society of Human Evolution conference in Liege, Belgium. I got the opportunity to meet a lot of old colleagues and friends and to attend talks on the latest evolutionary findings. Link for poster

Ups: networking, research exposure, conferences had different research focus, traveling

Downs: conferences too close to each other timewise, too many posters- next time presentation

Analyses

Various analyses were undertaken from samples of both the 2018 and 2019 expeditions in Umhlatuzana. All of the sediment analysis (granulometry, XRF, pH, LOI) is concluded and under preparation for publication. A total of 9 micromorphology thin sections were produced of the 2018 samples and are ready for analysis. Hopefully, the rest of the thin sections will have been prepared during the first half of 2020. 

Ups: interesting results, micromorphology samples not destroyed during shipping (!)

Downs: micromorphology thin section analysis delayed

 

Fieldwork

To begin with, I attended the Site Formation Processes field school in Athens, Greece organised by Takis Karkanas and Paul Goldberg. 

In July and August I participated in the Umhlatuzana excavation and took additional samples for micromorphology and other sediment analyses. In addition, a small fieldwork expedition was undertaken in Lesotho where I visited a Later Stone Age rock shelter, studied the stratigraphy and took some micromorphology samples.

Ups: balanced amount of time spend during fieldwork, lots of sampling

Downs: Needed one more week to reach bedrock in all the squares in Umhlatuzana!

reading 2020
Entering 2020 with no surprises since my fate was already foreseen!

South Africa Fieldwork 2019

Fieldwork is one of the best things when working in archaeology. Visiting new places, excavating exciting sites, meeting new people.

This year, our South Africa field season included all of the above! 

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ASAPA 2019 poster presentation

The first stop was the ASAPA archaeological conference that was held in Kimberley, Northern Cape. There, we presented a poster on first results of the stratigraphic assessment of Umhlatuzana rock shelter. We also got the chance to visit fascinating rock art sites in the area.

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Engraved rock art at WildebeestKuil and Nooitgedacht, Northern Cape, South Africa

 

Our excavation started shortly after. The team consisted of 7 people and we were regularly assisted by volunteers of the local archaeological society.

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Umhlatuzana rock shelter

 

This year we decided to undertake intensive sediment sampling in the excavated profile. The aim is to locate changes in geochemistry and mineralogy throughout the section in order to identify possible occupation signals and better assess the taphonomy of the site. We have so far conducted XRF, pH, and Magnetic Susceptibility analyses.

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Grid sampling
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XRF analysis undertaken at the University of Witwatersrand

 

Looking forward to an academic year analyzing all the data from this year’s fieldwork! 

 

Site Formation Processes Field School

I recently had the chance to attend a field school in Site Formation Processes of the Athenian Agora in Athens, Greece. It was organized by Takis Karkanas and Paul Goldberg through the Americal School of Classical Studies and the Wiener Lab

It was an amazing experience and gave the participants the chance to deepen our knowledge in aspects of geoarchaeology concerning formation processes of an urban archaeological site. Different scales of the site were discussed: the regional scale, the site scale, as well as the microstratigraphic scale.

 

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Looking at the broader picture: Geological section of fluvial deposits and palaeosoils in Boeotia, Greece

 

The field school combines both field (geomorphology, stratigraphy, sampling strategies) and laboratory (micromorphology, FTIR) training.

 

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Discussing the profiles within the Athenian Agora

In addition to the skillset acquired, the field school was a lot of fun and gave the opportunity to meet people interested in the same research field. It is organized annually (applications due ~April) and I would highly recommend it!

Sedimentology Lab visit

The Leiden GeoArch group organised a visit to the sedimentology laboratory at Leiden University College, Den Haag. The lab is led by physical geographer Peter Houben and fluvial geomorphologist Paul Hudson. There, they conduct various sedimentological analyses like grain-size analysis and pH measurements.

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Our visit started with an introductory session where Paul and Peter presented their work and research. We then moved on to the sedimentology lab where they showed us their facilities and talked about future plans for expanding the lab.

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Finally, we discussed the potential for collaboration in research and teaching.

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We hope that our visit will provide foundations for the development of a geoarchaeological connection between the Faculty of Archaeology (Leiden University) and Leiden University College.

Soil geochemistry on an early Swahili daub house, Zanzibar

I came across an interesting paper by Frederica Sulas and others (2019) who conducted a geoarchaeological study on an early Swahili (medieval) daub house at Unguja Ukuu, Zanzibaar (7th-14th c. AD). The study integrated geochemical, artefact distribution, and phytolith analyses. For the geochemical study pH, Loss on Ignition, and multi-element (ICP-MS) analyses were conducted on bulk sediment samples. The samples were derived from both the archaeological site (indoor and outdoor of the daub house structure) and the surrounding landscape. The main objective of the research was to investigate spatial organisation and activities within the house and test high-resolution systematic sampling strategies in this type of contexts.

 

View of the excavation trench and the 50 cm interval sampling grid (Sulas et al. 2019)

 

The use of multi-proxy geoarchaeological techniques helps to further explore the microarchaeological record that would otherwise not be visible with the naked eye. Various anthropogenic everyday activities leave microscopic and elemental traces that can be present even in seemingly homogeneous archaeological deposits. For example, this paper considers the use of Rare Earth Elements (REEs) as indicators of human remains (e.g. nails, skin, hair), seaweed, shell, sand, and animal manures (as ref. by Sulas et al. 2019, 34).

 

Distribution of Sm, V, Na, and K chemical concentrations (Sulas et al. 2019)

 

The REEs in this study reveal significant concentration patterning, and when combined with the other results can provide insight into the way people lived on the site, their subsistence strategies, and their spatial organisation. All in all, this paper showcases another example of how integrating various geoarchaeological techniques can develop a deeper understanding of various aspects of archaeological sites. 

 

Reference

Sulas, Kristiansen, and Wynne-Jones. “Soil Geochemistry, Phytoliths and Artefacts from an Early Swahili Daub House, Unguja Ukuu, Zanzibar.” Journal of Archaeological Science 103 (2019): 32-45.

Leiden GeoArch: New geoarchaeology group

Exciting news for the Faculty of Archaeology, Universiteit Leiden: a newly founded group, Leiden GeoArch, that plans to promote and discuss matters concerning geoarchaeology!

The first event will have the format of a lunch-lecture where Victor Klinkenberg will present his work on micromorphology of Mycenaean chamber tombs (March 4th/ 12h/ Van Steenis, Leiden).

What a wonderful opportunity to get inspired by various applications of geoarchaeological techniques to answer archaeological questions!

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Leiden GeoArch: Micromorphology of Mycenean Chamber Tombs poster

Various lectures and activities are on the schedule for the near future including my talk “Micromorphology for dummies” coming up May 6!

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Spring agenda 2019 for the LeidenGeoarch group: Faculty of Archaeology, Universiteit Leiden

 

Stay tuned!

Umhlatuzana 2018: Micromorphology Sampling

The micromorphological sampling of the Umhlatuzana archaeological site started after completing the excavation in mid-August 2018. In addition, bulk sediment samples associated with the micromorphological monoliths were collected. These are going to be processed for sedimentological, geochemical, and mineralogical characterization through various analyses like pH, Magnetic Susceptibility, grain size, Loss on Ignition, and Carbonate presence.

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Bulk sediment sampling

 

The size of the profile was approximately 1.5 m x 2.2 m. Only the west profile of the excavation was sampled; the remaining profiles were unstable and collapsing due to vandalizing incidents that happened in the past.

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Defining the location of the samples within the profile

 

The majority of the samples were collected using plaster bandages because of the high concentration of rocks in the sediments.

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Micromorphology sampling using plaster

 

Sampling with Kubiena tins was possible only on the upper, Holocene deposits. Six samples were collected using this method.  

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Micromorphology sampling using Kubiena tins

 

A total of 31 micromorphology samples were derived mostly focusing on layer boundaries and on what was assumed to be Pleistocene deposits.

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Umhlatuzana 2018 micromorphology samples

Umhlatuzana Rock Shelter Excavation 2018

My Ph.D. research within the “Finding resolution for the Middle to Later Stone Age transition in South Africa” project discusses scientific debates about the South African archaeology during the Pleistocene. The project is reexamining two archaeological sites located in KwaZulu-Natal (eastern South Africa), the Shongweni and Umhlatuzana rock shelters, both of which demonstrate occupational deposits during the Middle Stone Age to Later Stone Age transition. By determining the site formation processes, the geoarchaeological study aims to answer questions raised in relation to the archaeological contexts of the individual sites.

This blog entry shortly describes the fieldwork strategies we followed during the Umhlatuzana excavation (June-August 2018). A second blog post will follow describing the micromorphological sampling process.

Feedback, comments, and thoughts are highly welcomed.

strategies

The fieldwork strategies:

Step 1: Initial profile description

The first step was to identify and describe stratigraphic layers on the profile of the previous excavation. After producing an archaeological drawing, we compared our observations to the stratigraphic descriptions of the original excavation (Kaplan, 1990). We identified the units that were not clearly defined and established site-specific research questions.

Step 2: Excavation

The second step was to start excavating the stratigraphic layers (Single Context Excavation System) while keeping track of sediment changes. We excavated in 25×25 cm squares using ~2cm spits and documenting the relative location of finds larger than 2cm using a Robotic Total Station.

Step 3: Profile description

After the excavation, we re-identified the stratigraphic layers and units. This revised stratigraphic description was based both on the initial profile and the observations made along the excavation. Archaeological drawings of the new sections were produced.  

Step 4: Sampling Strategy

Based on the stratigraphic description we established the sampling strategies for chronological (OSL, radiocarbon), micromorphological, phytolith, and geochemical analyses. We focused on sampling specific sections that addressed our research questions. These sections included the MSA-LSA transitional deposits, poorly understood stratigraphic layers, and features with anthropogenic (hearths) or biological (bioturbation) input.

Reference

Kaplan, J. The Umhlatuzana Rock Shelter sequence: 100 000 years of Stone Age history. Southern African Humanities. 2, (1), 1-94.