This thesis compares the archaeobotanical remains from two Roman-era, Egyptian port sites: Berenike and Myos Hormos. A focus is put on the origin of the discovered materials, particularly in the...Show moreThis thesis compares the archaeobotanical remains from two Roman-era, Egyptian port sites: Berenike and Myos Hormos. A focus is put on the origin of the discovered materials, particularly in the context of the Silk Routes trade network of which these ports were a part. It concludes that Berenike seemingly had a larger focus on trade with Africa than Myos Hormos. Also, while both ports had Indian goods in their record, none seemed to have had a more pronounced focus on that subcontinent, although that was hypothesized beforehand. Furthermore, Berenike shows a decrease in the variety of goods traded after its period of inactivity in the 2nd and 3rd century, especially in regards to Indian goods. However, the variety and amount of local and African goods increased. The concurrent demise of Myos Hormos in this period did not seem to have an effect on the traded goods. Finally, this thesis served as a good example of how comparitive research beyond the level of the individual site could benefit the field of Silk Routes research, and which challenges this approach faces.Show less
Humans have been modifying landscapes in the southwestern Amazon for 10 000 years. Yet this modification did not comprise the intensive horticultural activities generally defined as ‘agriculture’...Show moreHumans have been modifying landscapes in the southwestern Amazon for 10 000 years. Yet this modification did not comprise the intensive horticultural activities generally defined as ‘agriculture’ within archaeological discourses. Instead of pursuing plant species’ domestication, local communities prioritised mixed-resource economies, in situ cultivation, and intentional biodiversity. These subtle but complex practices left a marked footprint on Amazonian soils, tree distributions, and biodiversity patterns. This thesis brings together palaeoenvironmental evidence of this footprint, to paint a picture of how humans managed landscapes in southwest Amazonia in the early and middle Holocene. It then approaches this ecological and archaeological data using anthropological theory and ethnographic evidence; these disciplines can (a) clarify the visibility of human-plant interactions in the eco-archaeological record, and (b) aid in interpreting what this record signifies about past lifeways. This transdisciplinary approach acknowledges the importance of considering cosmology when studying human-plant interactions, and how they can manifest materially. Human-nonhuman reciprocity is a prominent principle in many contemporary Amazonian ontologies, and is used in this thesis as a central paradigm for studying human ecological manipulations through time. Where conventional archaeological models of agriculture emphasise the central role of landscape domestication, the evidence from southwest Amazonia indicates that human horticultural activities comprised a process of active landscape co-creation. This thesis thus emphasises the need to rethink how we study human-plant interactions in archaeology, with critical implications for how we understand ‘agriculture’ as a whole – in Amazonia and elsewhere.Show less
Marathousa-1, Megalopolis basin, central Peloponnesus, dates to MIS 12 and is the oldest archaeological site in Greece. Palaeontological and archaeological finds include a near-complete skeleton of...Show moreMarathousa-1, Megalopolis basin, central Peloponnesus, dates to MIS 12 and is the oldest archaeological site in Greece. Palaeontological and archaeological finds include a near-complete skeleton of the elephant species Palaeoloxodon antiquus, many other animal bones and high amounts of stratigraphically associated small lithics. Cut marks on several bones indicate hominin exploitation of faunal resources. This research tried to assess the potential for plant exploitation at the site. In order to do that, the local vegetation of the site was reconstructed by means of a macro-botanical analysis. Two types of data were acquired: semi-quantitative data of four samples, and concentration data of one sample of those four. The results show that the majority of the identified plant taxa has an aquatic or waterside habitat, suggesting a lake-shore setting for the site. Big changes in the vegetation over time could not be established. Because not much is known about plant exploitation in the Palaeolithic, a literature study was deployed. By combining information from non-botanical sources and preserved plant remains at other sites, Palaeolithic plant use can be reconstructed. Plants must have played an important role in the lives of Palaeolithic hominins. Plants provided food, supplied raw material for tools, shelter and bedding and were essential for starting and maintaining a fire. Approximately two-third of the 62 plant taxa identified at Marathousa-1 is suitable for one or more of these purposes. The potential for plant exploitation at Marathousa-1 was therefore high, but due to the nature of the site and the sampling method actual use of plants by hominins at the site cannot be proven.Show less
Recent archaeological research in Oegstgeest, led by the Faculty of Archaeology of Leiden University, has revealed that the Merovingian settlement was active in the trade of crafts and agricultural...Show moreRecent archaeological research in Oegstgeest, led by the Faculty of Archaeology of Leiden University, has revealed that the Merovingian settlement was active in the trade of crafts and agricultural products that was probably produced in or near the settlement. To meet the demands of trade the local environment had to sustain these activities An understanding of the area surrounding the settlement is therefore necessary to gain insight into the cultural world of the Merovingians in Oegstgeest. A reconstruction of this environment may possibly contribute to the understanding of the dynamics between culture and nature. Plant macrofossils in a sediment sample from an excavated well in 2009 is analysed to study this environment. It demonstrates that the settlement was situated in a landscape with woodlands, dry and damp grasslands, dunes, mudflats, and water sources such as swamps, channels and (side-)rivers.Show less
Archaeobotanical investigation of the amount of salt-influx in the Rhine estuary, on material from sites between Dorestad and Katwijk, dating between AD 500 and AD 1500.
On the beach of Happisburgh iron rich blocks have been washing up for centuries. When an iron mineralised faunal fossil with cut marks was found, this formed the direct occasion for further...Show moreOn the beach of Happisburgh iron rich blocks have been washing up for centuries. When an iron mineralised faunal fossil with cut marks was found, this formed the direct occasion for further investigation. The iron rich blocks are filled with plant macro and other fossils. In the nineteenth century Clement Reid and six others reported similar iron rich blocks washing up. They named the presumed locality the ‘Elephant Bed’ after the many Elephant fossils yielded from the same deposition. This thesis investigates the plant macro fossils and a basic lithological analysis of 66 iron rich blocks collected from Happisburgh Site 5 in 2012 by dr. M.H. Field in an attempt to establish a palaeoenvironmental reconstruction that could indicate possible habitability of early hominins. In order to do so this research has been placed in the context of East Anglian, Pleistocene research on the stratigraphy. This sequence is extremely complex and has been revised, including Reid, West, Lee, Hamblin and others. Not only are there now two opposing views on the classification of these sediments, the associated ages differ by several Marine Isotope Stages. Some general consensus has been achieved on the palaeogeography, namely the presence of ancient rivers in this part of England. Whether this be the ancient Thames or a local river called Bytham remains a discussion. Fluvial sediments are known for depositing iron rich blocks. Several sites in East Anglia have yielded flaked artefacts, such as Pakefield and Happisburgh Site 3, but no human fossil remains. Happisburgh has four other sites other than the one investigated for this thesis, that have all yielded some form of evidence for hominin presence (i.e. cut marks, flaked artefacts). Clement Reid of the British Geological Survey, Peter Murphy of the English Heritage and Simon Parfitt of the Natural History Museum have, respectively published and shared, plant macro fossil results for these iron rich blocks. The fossils included aquatic and woodland taxa. Murphy’s methodology is different from the methodology used for this thesis. Both methods have their pros and cons, and depending on the research questions one or the other may be used in future investigations. The iron rich blocks have underwent severe taphonomic processes that have had their influence on the preservation of the botany, and possibly had an effect on over- or underrepresentation of the taxa. Results from the lithological analysis indicate the existence of several different facies, indicating the presence of both a river as a wetland or horse shoe shaped lake. The plant macro fossils indicate aquatic taxa, terrestrial taxa and woodland taxa. Some faunal remains have been found, such as shell impressions and one fossilized abraded mammal long bone. The shell impression identification corresponds with identifications made by both Reid as Murphy and suggest reasonably clear, stagnant or mild flowing fresh waters. In the absence of an in situ locality for these blocks, several inferences can be made based on the presented results. Three scenarios are described, order from most likely to least likely. The final conclusion attests the hypothesis, as there seems to be a clear indication for a temperate environment that could possibly have been a habitat for early hominins.Show less
