DHSC Project Team: Francis Stankiewicz, Flinders University

F1

My interests have always revolved around a love for the ocean, the arts and archaeology. As an undergraduate at Coastal Carolina University (USA), I majored in marine science with two minors, coastal geology and art history. I became interested in how geophysical techniques could add a new dimension to studying marine environments in support of marine geological and maritime archaeological research. In particular, I became interested in prehistory and the environmental influences that affected early cultures. At the moment, I’m working as a marine geologist in Florida while I do my MA in maritime archeology through Flinders. Luckily, modern day technology allows external students to stay in close communication with fellow researchers, which is important.

F2

The research team here in Denmark is extraordinary; it’s made up of everything from geomorphologists and geoarchaeologists to coastal prehistorians and specialists in Ertebølle culture. Along with Dr Paul Baggley (CTO at Wessex Archaeology and Adjunct Lecturer in Maritime Archaeology at Flinders), my job is to run the geophysical equipment (sidescan sonar and a sub-bottom profiler) which will give us a better understanding of the site’s submerged surface and subsurface. Although Horsens Fjord is protected on all sides from major weather events, which gives the appearance of calm waters, undertaking work on the site has proven to be a challenge. Weather and sea conditions have not been particularly favorable; certainly not ideal for geophysical or diving operations. As we ran our survey, we had to dodge boulders hidden just below the water’s surface while making sure we didn’t run aground in the shallower waters. As with all research, you persist and we were able to collect great data in the end.

F3

After completion of the geophysical operations, I joined the scientific dive team. We excavated the midden in one meter increments, carefully sifting through the material for further analysis. Now the real fun begins: data processing and writing. It’s going to be a big job. The geophysical data will be processed and interpreted based on its returned signals and ground truthed samples (geological samples) collected by other members of the Deep History of Sea Country (DHSC) project team Dr. Ingrid Ward and Peter Ross, as well as scientists at Moesgaard Museum. In terms of the environmental analysis from the site, the geophysical survey, aerial survey, geotechnical data and excavations will be used in combined efforts for further interpretations, we should know by the end of the year what we got.

____

As the months progress over this next year, we will work to finalize our data findings in support of next season’s field operations. It is an exciting venture to view the archaeological information as the site reveals itself with further data analysis. I look forward to working with the DHSC research team next season to dig further into the wealth of knowledge which still lays submerged beneath the sea’s surface.
F4

DHSC Project Team: Peter Ross, Flinders University, PhD Candidate

Having completed my Masters in Maritime Archaeology at Flinders in 2009, I began as a PhD candidate for the Deep History of Sea Country project in March of this year. In between, I’ve been working in cultural heritage management in my home country of Canada, with occasional forays into research-based digs in Europe. My particular interest is to study the formation, degradation, and erosion of archaeological features that have been subjected to one or more episodes of sea-level transgression. Understanding the effects of these phenomena will help allow us to identify archaeological features during underwater investigations in Australia.

PR1a

I am in Denmark to help excavate a transgressed shell midden on the island of Hjarnø, and to study whether analyses of associated lithic materials could aid in that interpretation. Denmark is known for its approximately 500 shell middens from the Mesolithic period, and about the same number from the Neolithic. During the week prior to our excavation I visited some of the documented shell midden sites throughout Jutland in an attempt to get an idea of how these massive archaeological features might react to transgression. Of course, I also found time to visit the incredible Moesgaard Museum, for a side trip to Silkeborg to view the famous Tollund Man, and to visit numerous ship burials. There is so much amazing archaeology in Denmark, and a great place to study shell middens!

PR2a

My time on Hjarnø has included many tasks. In addition to the excavation of a transgressed shell midden, I’ve been involved with using sidescan sonar for identifying underwater sediments and geology, collecting core samples for more detailed sediment assessment, the seemingly endless collection of photos for building photogrammetry models, geological observations of eroding cliff faces, and archaeological surveys of beach areas.

PR3a

——

We’re going to finish our work on Hjarnø in the next few days, but look forward to our return next year. I’ve decided to stay in Denmark for an extra week though in order to immerse myself in the archaeological library at Mosegaard Museum. Our colleagues at Moesgaard have also invited me to participate in the excavation of a submerged log-boat, dated to around the same time period as the formation of many of the shell middens I’ve been studying.

PR4a

DHSC Project Team: Dr Ingrid Ward, Geoarchaeologist

IMG_7141

I have a Scandanavian name and, for most of my life, my hair has been blonde (now going grey), so often people ask whether I have any family here in Denmark. The answer is no, my origins are Australasian (Aussie and Kiwi). Where I come from the land is more red and yellow, not green; the water is warm, not freezing; there are sharks and stingers (jellyfish) in the water; there are no thick peat (gyttja) deposits, it’s mostly carbonate; and there are no known submerged prehistoric marine archaeological sites. Therein lies the reason we are here.

We are here to excavate the only known submerged prehistoric midden site in the world, and learn how we might apply such knowledge in an Australian context. As if that isn’t daunting enough, getting into the 15°C water. Not helping are the unseasonably cold and windy conditions – the spirit is willing, but the flesh is weak.

P1040138

In the first snorkel over the site, during a brief window of sunshine, we see flint artefacts everywhere! Perhaps not surprising given we have already observed numerous flint artefacts just washed up on the shoreline. Our Danish colleague, Peter Moe Astrup, swims up to me holding a bit of a wooden handle that he has just found – probably hazel he says. A few minutes later he shows me a worked reindeer bone, showing an edge on which an axe head was hafted. On another day, Peter picks up a bit of an early Ertebolle (c. 6.8 – 6.4 ky BP) ceramic – made from a mix of granite and the glacial marine clay over which the midden site has accumulated. It’s almost ridiculous but, then again, people have been researching submerged Mesolithic settlements in Denmark for over 40 years. We are mere novices in Australia.

As we dive and begin to excavate the midden site itself, we observe a dense layer of large, flat oyster shells, with patches of black charcoal and ash – a hearth. I’m having to rethink how I’m going to get an undisturbed profile or sample any sediments under water. It’s all new territory and we are all learning as we go. I am constantly aware of the privilege we have here, but all the time wishing it could just be a little bit warmer!

—-

Dr Ingrid Ward is a geoarchaeologist. She is also a trained commercial diver and experienced Australian archaeologist now focused on the submerged continental shelf. Ingrid is the dedicated DHSC Postdoctoral Researcher and will work on both European and Australian components of the project.

P1040150

DHSC project team guest post: Prof. Geoff Bailey

From time-to-time, our Project Blog will feature guest posts from specific team members or project partners. Our first of such posts comes from Professor Geoff Bailey of the University of York (UK) and Flinders University of South Australia (and the senior member of the DHSC project leadership). 

DHSC project team guest blog post: Prof. Geoff Bailey

For someone who has spent half a lifetime looking at shell middens and shell mounds in many parts of the world, and in recent years has attempted to find underwater examples offshore of known shell mounds on land, so far without success, this week on the Danish island of Hjarnø has introduced me to my first experience of a genuine submerged shell midden deposit.

GB 5

The first sign of the underwater midden from land is an intertidal zone exposed at low tide and littered with flint artefacts and shells. The location is close inshore in shallow water on the edge of a channel, between the island and the mainland just 600 m away. This is exactly the sort of location expected according to Anders Fischer’s fishing site model. The sceptic in me wonders if the intertidal material has been eroded downslope from a mound that once stood on the ridge behind the modern beach. My Danish archaeological colleague Peter Moe Astrup, who first excavated the site seven years ago, assures me that this is material from the surface of a submerged midden just 20 metres further out under water. Some of this shell deposit is protected under a layer of peat and sand, but some has become exposed. It is material from here that has been gently washed ashore by tidal currents. Since the excavation of the submerged shell midden revealed an in situ hearth in the shell deposit, and bones of fish and land mammals and artefacts of flint, bone and antler typical of the classic Ertebølle, I am persuaded that the underwater deposit must be a pre-inundation in situ deposit.

The site itself is some 20 metres further out in shallow water scarcely more than a metre deep, so it is quite easy to inspect the surface of the site visible on the seabed. The shell midden layer shows large oysters, cockles and mussels, typical of shells collected for food, shell fragments and a dense litter of flint artefacts, mostly with fresh and unpatinated surfaces. But here’s another surprise. There are also large numbers of large shells of species not present in the prehistoric midden – razor shells and a species of large, thin-shelled clam. Moreover, some of the cockle shells are clearly of modern animals. This becomes apparent when I pick up a large cockle with the pair of valves intact and shut – not unknown in archaeological middens – only to find, after prising the valves apart, a live animal inside. So, the surface of the ancient midden is a mixture of modern and ancient shells from very different periods of time – in short, our familiar friend a palimpsest. Telling the modern shells that have died naturally from the prehistoric ones collected as food is not at all easy, and would be even less so when coming across a shell deposit elsewhere on the seabed with no prior knowledge. The gjytta layers are even more interesting. Peter points out a half-buried antler axe, fishes up a neatly cut segment of round hazel wood, and casually asks me to watch out for a sandbag that is protecting a partly emerged wooden log boat. What wouldn’t I give to find evidence like this in any of the other parts of the world where I have worked? Yet here in Denmark it is a struggle to get sufficient funding to do justice to the recovery of this remarkable material.

GB 4

Another first for me is that I was persuaded to don a dry suit to go into the water and take a closer look. For the uninitiated like me, a wet suit lets some water through to keep a thin layer of warming water against the skin. A dry suit keeps you and your underclothes completely dry, or at any rate it is supposed to. Since I’m borrowing somebody else’s dry suit, I discover that I’ll have to take off some of my ordinary day clothes to struggle inside this rubbery ‘onesie’ garment, immediately risking the sacrifice of warmth for access. This is Denmark in early summer, much like home in England – cold, wet and windy most of the time with occasional spells of blue sky and bursts of sun. The rubber seal at the holds my throat in a near strangulating grip. I am given a safety brief on how to recover if I fall underwater and all the buoyant air in the suit goes to the feet. Not for the first time, I wonder what I am letting myself in for in taking part in an underwater archaeological project. Once in the water and submerged up to my chest, I hold a stake attached to a guideline for the best part of an hour while John McCarthy holds the other end 50 m away and keeps an eye on my progress. Jonathan Benjamin swims over the seabed with a snorkel and a camera to create a map of the seabed surface. I find myself continuously fighting to keep my footing against the power of the waves and the wind as I move the stake to the next point on the grid. But I know, as a conventional land-based archaeologist, that I cannot begin to understand what is involved in underwater work without participating in this way.

GB 3

Much of the first few days have been like any other field project – trying out equipment to discover what’s missing or doesn’t work, adapting to local conditions, and working out by trial and error the best way to do things. For an underwater project, these uncertainties are amplified by the added logistical complexities associated with boats, underwater equipment and the vagaries of changing weather, tidal currents, wind and waves. A first spell of survey with a sidescan sonar on a small boat is aborted because the rain sets in and the laptop supplied with the equipment is not a waterproof model, the battery charger on one of the underwater video cameras is playing up, and a first attempt at underwater video photography over the site area has to be abandoned because of poor visibility. The drone has been damaged in transit and needs to be looked at by the nearest service agent. Civilisation in the form of wifi and other vital supplies lies on the mainland a short ferry-ride away.

Next day we try again but have to wait for the tide to change. Much time is spent standing around waiting for conditions to improve, but the time is not entirely wasted – we talk about the finer points of archaeological modelling and the purpose of archaeological theory. Later in the day we get a parking ticket on a shopping trip to the nearest town because we couldn’t read the regulations in Danish, and one of the rooms where we are staying has sprung a leak in the ceiling after a burst of heavy rain.

GB 6

By day three, things are beginning to settle down, some sort of daily rhythm is becoming established, new data is coming in and getting processed, and everyone in our small team is getting on with a sense of purpose with what needs to be done.

The moral of this short saga is a familiar one for anyone used to archaeological fieldwork in unfamiliar locations. Expect that anything that can go wrong will go wrong. Be prepared. And above all be patient!

Professor Geoff Bailey is Anniversary Professor of Archaeology (Emeritus) at the University of York, UK and a Senior Research Fellow at Flinders University, South Australia. He is an expert in human exploitation of shellfish, coastal prehistory and the archaeology of submerged landscapes. He also cooks a mean chicken curry.

GB 1

Earliest Australians enjoyed a coastal lifestyle

File 20170510 7921 1tzv3vh
Three main excavation squares within Boodie Cave.
Peter Veth, Author provided

This piece originally was originally published in The Conversation by members of the DHSC project team: 

Sean Ulm, James Cook University; Ingrid Ward, Flinders University; Peter Veth, University of Western Australia, and Tiina Manne, The University of Queensland

Archaeological excavations in a remote island cave off northwest Australia reveal incredible details of the early use by people of the continent’s now-submerged coast. The Conversation

Out latest study reveals that at lower sea levels, this island was used as a hunting shelter between about 50,000 and 30,000 years ago, and then as a residential base for family groups by 8,000 years ago.

As the dates for the first Aboriginal arrival in Australia are pushed back further and further, it is becoming clear how innovative the original colonists must have been.

The earliest known archaeological sites so far reported are found in inland Australia, such as Warratyi rock shelter in the Flinders Ranges and Madjedbebe in Arnhem Land. These places are a long way from the sea, and were once even more so when past sea levels were lower and the coast even more distant.

But we do know that the earliest Australians were originally seafarers. They came from island southeast Asia and no matter which route they followed had to make sea crossings of up to 90km to get here.

The earliest landfall on the continent is now likely to be at least 50m below the present ocean. Until now we have known very little about these first coastal peoples.

Our research, published this week in Quaternary Science Reviews, begins to fill in some of these gaps.

Island dig

For the past five years an international team of 30 scientists has been working in collaboration with the Buurabalayji Thalanyji Aboriginal Corporation and Kuruma Marthudunera Aboriginal Corporation on Boodie Cave, a deep limestone cave on the remote Barrow Island, off the Western Australia coast.

Since the initial early dates for Boodie Cave were reported in 2015, our team has been forensically analysing the archaeological and palaeoenvironmental remains, as well as re-dating the site to build up a robust picture of the lives of the people who lived here.

PhD student Fiona Hook at the Boodie Cave excavation.
Kane Ditchfield

The results from radiocarbon and optically stimulated luminescence dating techniques from four independent dating laboratories show that Boodie Cave was first occupied between 51,100 and 46,200 years ago.

These dates make Boodie Cave one of the earliest known locations in the settlement of Australia and the earliest site anywhere near the coast.

Project leader Peter Veth discusses the significance of the Boodie Cave discoveries.

Mainland connection

When Boodie Cave was first occupied, Barrow Island was part of the mainland, with the shoreline between 10km and 20km further west.

The shoreline became even more distant as the planet moved into an ice age and sea levels dropped to 125m below present, around 20,000 years ago. Shortly thereafter global temperatures warmed and, as the ice melted, sea levels rose quickly.

Throughout this long period people returned again and again to Boodie Cave. The limestone that forms the cave provides ideal conditions for preservation, giving us incredible details about the people who lived there.

The cave contains one of Australia’s longest dietary records. These animal remains provide us with profound insights into what people were hunting and collecting from initial settlement onwards, and how they adapted to a new and ever-changing arid landscape.

PhD students Jane Skippington and Kane Ditchfield sorting material excavated from Boodie Cave.
Bob Sheppard

Besides wallabies, kangaroos and other terrestrial animals, the archaeological deposits contain marine shells transported from the distant coast.

In the deepest levels, when the shoreline was 20km or so distant, there are only four different types of shellfish that we have directly radiocarbon dated to 42,300 years ago. These shells represent the first direct evidence of marine resource use in Australia, and some of the earliest in our region.

Marine shell dating up to 40,000 years ago was excavated from Boodie Cave, including this baler shell artefact dating to around 6,800 years ago.
Fiona Hook

With rising sea levels the coastline came closer to the cave and the number and variety of marine resources increased exponentially.

By 8,000 years ago, there are 40 different types of marine shells as well as exceptionally well-preserved remains of sea urchin, mud crab, reef fish, marine turtle, marine mammal and a variety of small and medium-sized terrestrial animals.

By 6,800 years ago the cave and the whole island was abandoned as rising sea levels finally cut it off from the mainland.

Hunting shelter

We argue that Boodie Cave was used as an inland hunting shelter between about 50,000 and 30,000 years ago before becoming a residential base for family groups by 8,000 years ago.

Dietary remains in addition to shell artefacts, incised shells, shell beads and thousands of stone artefacts show that Boodie Cave was a frequently visited location on the landscape.

Boodie Cave is located on the second bluff in the centre of the photograph.
Kane Ditchfield

Our study clearly shows that not only were Aboriginal people continuing to use marine resources across a period of dramatic environmental change, but they were also exploiting a range of desert resources. This demonstrates a successful adaptation to both the coasts and deserts of northern Australia.

Recent genetic studies suggest that colonisation was coastal, with people rapidly moving around the east and west coasts of Australia before meeting up in modern South Australia.

But the coasts along which the earliest Australians traversed were very different to today’s, not only in terms of ecology but also in distance. In some places the earlier coastline would have been hundreds of kilometres from its present position.

Peter Veth (left) with Thalanyi elders Anne Hayes, Roslyn Davison and Jane Hyland at Boodie Cave on Barrow Island.
Peter Veth

Sea levels rise

Over the past 20,000 years sea level has risen 125m, submerging the continental shelves surrounding Australia and separating the mainland from New Guinea and Tasmania.

Our findings provide a unique window into the now-drowned Northwest Shelf of Australia.

Lead archaeologist Peter Veth excavating a rich layer of dietary remains and artefacts below the surface of Boodie Cave.
Kane Ditchfield

Boodie Cave provides the earliest evidence for coastal living in Australia and gives us an indication that coastal resources have been important to people since initial colonisation.

Nearly one-third of Australia’s landmass was drowned after the last ice age and along with it evidence for coastal use by some of the earliest Australians.

Thousands of archaeological sites have been recorded on the continental shelves of Europe, Asia and the Americas, but no submerged prehistoric sites have been reported anywhere off Australia.

These submerged landscapes of Australia open up an entirely new frontier of archaeological research and will shed even further light on the lives of the first people to arrive on Australian shores.

Sean Ulm, Deputy Director, ARC Centre of Excellence for Australian Biodiversity and Heritage, James Cook University; Ingrid Ward, Post-Doctoral Research Fellow on the ARC DP Deep History of Sea Country project administered by Flinders University, Flinders University; Peter Veth, Professor of Archaeology, University of Western Australia, and Tiina Manne, ARC DECRA Research Fellow, The University of Queensland

This article was originally published on The Conversation. Read the original article.

Welcome to our project blog!

Deep History of Sea Country: Climate Sea level and Culture

Funded by Australian Research Council (Discovery Project DP170100812)

Submerged landscape archaeology is an under-researched field in Australia and represents a major opportunity to address knowledge gaps in world prehistory such as early human migrations, the archaeology of land bridges and coastal-hinterland cultural exchange.

 

Welcome to our project blog!

This is our blog where we hope to post regular updates on our project as we begin our research on the submerged landscape archaeology of Australia and beyond!

Submerged landscape archaeology is an under-researched field in Australia and represents a major opportunity to address knowledge gaps in world prehistory such as early human migrations, the archaeology of land bridges and coastal-hinterland cultural exchange.

Project Team and Partner Institutions

 

Deep History Logo V8

Nearly one-third of Australia’s landmass was drowned after the last ice age and generations of people were displaced by sea-level change. This pioneering, multi-disciplinary study of submerged landscape archaeology in Australia is designed to investigate the records of the now-submerged Pilbara coast (spanning 50,000 to 7000 years ago). Information from drowned contexts will help address critical debates in Australian archaeology relating to past sea-level rise, population resilience, mobility, and diet. The project integrates cultural and environmental studies and contributes a unique southern hemisphere insight into world prehistory. Further, an adaptation of method from the world’s only confirmed submarine middens, in the Baltic Sea of modern Denmark, will contribute to broader questions of site submergence and preservation as well as cultural response to rising sea levels and shifting shorelines. A suite of cutting edge marine and aerial survey techniques will be developed to investigate physical and cultural submerged landscapes.