Cited by 3Archaeology and ancient environmental studiesSoil and Environmental StudiesArchaeological and Geological Studies

The DOI matches its Crossref record; 68 of the 68 references it cites were found in a registry or an index; none of the 6 sources its claims cite is checked for support yet.

Modelling Prehistoric Topography and Vegetation in the Lower Thames Valley, UK: Palaeoenvironmental Context for Wetland Archaeology and Evidence for Neolithic Landnám from North Woolwich

Open access
Stastney, Phil, Scaife, Rob, Carretero, Lara Gonzalez, Whittaker, John E., Cameron, Nigel, Allison, Enid·2023·Environmental Archaeology

Abstract

Multi-proxy investigations at 2 Pier Road, North Woolwich, London, UK, have revealed deposits spanning the Middle-Late Holocene from the late Mesolithic (c. 4360 cal BC) onwards. Pollen data show an Elm Decline at c. 4210–3950 cal BC followed by landnám clearances at c. 4210–3910 cal BC and c. 3710–3030 cal BC and the first appearance of cereal at c. 3540–3030 cal BC. These events are potentially contemporary with the construction of nearby Neolithic trackways, providing indirect evidence for agriculture and settlement. REVEALS modelling shows the first significant reduction in woodland cover is coincident with the Neolithic Elm decline, but the main step-change to open conditions occurred in the Early Bronze Age, following a decline in lime at c. 2110–1630 cal BC. Palaeo-topographic modelling of the region shows that although the trend towards increasing openness coincides with gradual wetland expansion, the shift to open vegetation cover cannot be explained by this and is probably the result of human activity. This study highlights the value of combining deposit and vegetation cover modelling to contextualise wetland archaeology and shows that together these provide useful proxies for landscape-scale human activity that can identify ephemeral signals of prehistoric activity.

Overview

AI snapshot

Written from the paper’s full text.

TL;DR

Multi-proxy work at 2 Pier Road, North Woolwich, reconstructs Middle–Late Holocene environments and finds Neolithic Elm Decline/landnám signals, later Bronze Age woodland opening, and wetland expansion in the Lower Thames Valley. Combining deposit and vegetation-cover modelling contextualises nearby prehistoric trackways and suggests later prehistoric openness was mainly human-driven.

Key findings

  • Pollen data span the late Mesolithic from c.4360 cal BC, with an Elm Decline at c.4210–3950 cal BC, landnám clearances at c.4210–3910 cal BC and c.3710–3030 cal BC, and first cereal pollen at c.3540–3030 cal BC.
  • REVEALS modelling shows mixed deciduous trees and shrubs dominated in the Late Mesolithic and persisted through the Neolithic; grassland expanded in the Early Neolithic mainly through Ulmus reduction (15% to 7%), with cultivation first apparent in 3500–3000 BC.
  • The main step-change to open vegetation (>60% grasses/herbs) occurs from c.2000 BC in the Early Bronze Age, with a sharp Tilia reduction (23% to 5%); this follows the Lime Decline dated to c.2110–1630 cal BC.
  • Palaeo-topographic flooding models show gradual wetland expansion, and known trackways plot close to modelled marginal wetlands; the shift to open vegetation cannot be explained by wetland expansion alone and is probably due to human activity.

Methods

  • Museum of London Archaeology geoarchaeological investigations at a 0.17 ha site; four windowless boreholes (BH01–BH04) reached the base of the Holocene sequence, with BH03 sampled for plant macrofossils, radiocarbon dating, pollen, diatoms, ostracods, foraminifera and testate amoebae, and BH01/BH04 bulk samples for insects.
  • Seven AMS radiocarbon dates from BH03 were calibrated using OxCal 4.3 and IntCal13; a Bayesian age-depth model used Bacon, and a deposit model of the pre-Holocene surface used Kriging constrained by LIDAR.
  • Regional vegetation cover was reconstructed with REVEALS via REVEALSINR in DISQOVER, using 500-year time-slices; wetland expansion was modelled by “flooding” the Early Holocene surface using the site age-depth model and existing Lower Thames relative sea-level models.

Limitations

  • Stated: precise sea-level index points are scarce, so the relative sea-level models used for flooding are provisional and schematic; the age-depth model has a mean uncertainty of 386 calendar years (s.d. = 92), ranging from 567 years at 7.80 m b.g.l. to 211 years near the top.
  • Stated: a possible outlier date (SUERC-88163) is largely excluded by the age-depth model; a hiatus is inferred between c.1312–967 cal BC and c.151 cal BC–cal AD 188, and the period 1000 BC–AD 1 was not modelled due to this hiatus.
  • Stated: pollen counts were sometimes limited, with totals of 200–350 total land pollen grains; evident from the text, the main multiproxy sequence relies on a single core (BH03), and prehistoric occupation evidence in the region is described as fragmentary due to later urban truncation.

Model-written summary. Check it against the paper before relying on it.

Integrity signals

Registry

Crossref · 10.1080/14614103.2021.1880683

Cites

68 of 68 references verified0 citation errors · 0 not checkable

Statistics

Nothing to recompute.

Figures

Image 1
CC-BY-NC · From the PDF
Figure 1 Site location.
Figure 1 Site location.CC-BY-NC · From the PDF
Figure 2 left: superficial geology of the vicinity of the site; right: modelled Early Holocene surface.
Figure 2 left: superficial geology of the vicinity of the site; right: modelled Early Holocene surface.CC-BY-NC · From the PDF
Image 4
CC-BY-NC · From the PDF
Figure 4 Micropalaeontology from BH03. Values of various microfossils are given on a 4-point scale of abundance (0 = absent; 3 = abundant).
Figure 4 Micropalaeontology from BH03. Values of various microfossils are given on a 4-point scale of abundance (0 = absent; 3 = abundant).CC-BY-NC · From the PDF
Figure 5 Percentage pollen diagram from BH03, 2 Pier Road.
Figure 5 Percentage pollen diagram from BH03, 2 Pier Road.CC-BY-NC · From the PDF
Figure 6 Modelled expansion of wetland in the study area in 500 year-time slices from the Late Mesolithic (4500 -4000 BC) up to the Late Bronze Age (1500 -1000 BC) and during the Roman period (AD 1 -500). See Table 5 for details of archaeological features.
Figure 6 Modelled expansion of wetland in the study area in 500 year-time slices from the Late Mesolithic (4500 -4000 BC) up to the Late Bronze Age (1500 -1000 BC) and during the Roman period (AD 1 -500). See Table 5 for details of archaeological features.CC-BY-NC · From the PDF
Figure 7 Stacked bar chart showing modelled regional vegetation cover in 500 year time-slices.
Figure 7 Stacked bar chart showing modelled regional vegetation cover in 500 year time-slices.CC-BY-NC · From the PDF

Verification

Claims the paper makes

28 Own result · 21 Own interpretation · 6 No basis given · 5 Not checked yet · 2 No full text of the sources · 1 Sources not found · 1 Own method

Show all 43 claims

  • It may state two separate claims as one. 18
  • Probably not a substantial claim. 5
21 of 21
  • The paper relies on this without support.

    The assumptions of the REVEALS model are met for the Pier Road pollen data after excluding autochthonous taxa such as Alnus and Cyperaceae.

    “Autochthonous plant taxa such as Alnus (alder) and Cyperaceae (sedges) were excluded from the model to avoid violating the assumptions of the REVEALS model”
  • The paper relies on this without support.

    The modelled extent of marginal wetlands accurately represents the actual extent of wetlands at the relevant time-slices.

    “this model indicates that this site would have been at the edge of the floodplain at the time of construction during the Neolithic.”
  • The paper relies on this without support.

    The modelled vegetation cover accurately represents past vegetation cover in the study area.

    “with the increased number and spatial spread of trackways in the Bronze Age coinciding with modelled decline of woodland cover from about 2000 BC onwards.”
3 of 3

Self-check

Percentages, sums and reported differences re-computed from the paper’s own numbers.

Each contradiction between two passages listed here was confirmed by an independent check.

3 of 3

Citations

Cites

Show all 68 references

Research works printed but not linked: 28

  1. Bates J., 1999, London Archaeologist, 8, 325
  2. Bates M., 2004, Towards a New Stone Age: Aspects of the Neolithic in South-East England, 50
  3. Bennett K. D., 1994, Quaternary Newsletter, 73, 1
  4. BGS, 1998, Dartford. England and Wales Sheet 271. Solid and Drift Geology, 1:50,000
  5. Bridgland D. R., 2014, The Quaternary of the Lower Thames & Eastern Essex
  6. Carew T., 2009, London and Middlesex Archaeological Society Transactions, 60, 1
  7. Carey C., 2018, Deposit Modelling and Archaeology, 3
  8. Chapman H., 2013, Modelling Archaeology and Palaeoenvironments in Wetlands: The Hidden Landscape Archaeology of Hatfield and Thorne Moors, Eastern England
  9. Charman D. J., 2000, The Identification of Testate Amoebae (Protozoa:Rhizopoda) in Peats
  10. Coles B., 1989, People of the Wetlands
  11. Devoy R. J. N., 2000, Coastal Change During Sea-Level Highstands: The Thames Estuary, 40
  12. Divers D., 1994, Archaeological Excavation of the Former Beckton Nursery.
  13. Divers D., 1994, Archaeological Investigations of Hays Storage Services Ltd, Pooles Lane, Ripple Road, Dagenham, Essex.
  14. Godwin H., 1975, The History of the British Flora
  15. Hartley B., 1996, An Atlas of British Diatoms
  16. Hustedt F., 1953, Sv. Bot. Tidskr, 47, 509
  17. Hustedt F., 1957, Ab. Naturw. Ver. Bremen, 34, 181
  18. Iversen J., 1941, Danm. Geol. Unders, 11, 1
  19. Jessop L., 1986, Dung Beetles and Chafers. Coleoptera: Scarabaeoidea, Part 11. ed, RES Handbooks for the Identification of British Insects.
  20. Jones A. P., 1999, The Description and Analysis of Quaternary Stratigraphic Field Sections., 27
  21. Krammer K., 1991, Bacillariophyceae
  22. Merriman N., 1987, London Archaeologist, 5, 318
  23. MOLA, 2019, 2 Pier Road, North Woolwich, London E16: Geoarchaeological Post-Excavation Assessment and Updated Project Design, Unpublished Report
  24. Moore P. D., 1991, Pollen Analysis
  25. Raftery B., 1996, Trackway Excavations in the Mountdillon Bogs, Co. Longford, 1985–1991
  26. Stafford E., 2012, Landscape and Prehistory of the East London Wetlands: Investigations Along the A13 DBFO Roadscheme, Tower Hamlets, Newham and Barking and Dagenham, 2000–2003
  27. 10.3318/priac.2020.120.02 · DOI
  28. White I. M., 1982, Psylloidea (Nymphal Stages) Hemiptera, Homoptera, Part 5 (b). ed, RES Handbooks for the Identification of British Insects.

Metadata

Authors
Stastney, P., Scaife, R., Carretero, L. G., Whittaker, J. E., Cameron, N., & Allison, E.
Affiliations
  • Museum of London Archaeology (GB)
  • University of Southampton (GB)
  • Museum of London Archaeology (MOLA), London, UK
  • Natural History Museum (GB)
  • University College London (GB)
  • Canterbury Archaeological Trust (GB)
Corresponding author
Stastney, Phil
Venue
Environmental Archaeology
Published
2021-02-11
Volume
28
Issue
3
Pages
133-149
ISSN
  • 1461-4103 (ISSN-L)
  • 1749-6314
OpenAlex
W3131620238
Cited by
3
References
68
Citations by year
2026: 1 · 2023: 1 · 2021: 1
FWCI
1.18
Type
journal article
Language
en
Open access
Licence
cc-by-nc
Locations
  • Environmental Archaeology (publishedVersion)
  • Apollo (University of Cambridge) (submittedVersion, cc-by-nc)
  • RePEc: Research Papers in Economics (submittedVersion)
  • ePrints Soton (University of Southampton) (submittedVersion)
  • Apollo
Funders
Higgins Construction Ltd
Topics
  • Social Sciences › Archeology › Archaeology and ancient environmental studies
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil and Environmental Studies
  • Social Sciences › Arts and Humanities › Archeology (arts and humanities) › Archaeological and Geological Studies
Keywords
elm decline, wetland archaeology, paleotopography, paleovegetation, pollen analysis, woodland clearance, cereal cultivation, Early Bronze Age

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