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Mesolithic to Bronze Age landscape signatures during periods
of abrupt climate change: current work from the Upper
Vinalopó Valley (SE Spain) lake deposits
Marie-Curie Intra-European
Fellowship: IEF-628589
Dr. Samantha E Jones; Prof. Fransesc B Casas; Dr. Javier Fernández- Lopez de
Pablo
50
100
150
200
250
300
350
400
Depth
D
ecora
te
d
fo
re
stty
pes
20
Facet
ate
Fore
stty
pes
Sedge
pattern
ed
&
w
ithoutapic
es
Sedge
bulli
fo
rm
s
w
ith
hor
ns?
G
ra
ss
bullifo
rm
ssm
ooth
to
p
Pooid
eae
bilo
ba
te
s
H
atbi
lo
bate
s
Tw
o
poi
ntbi
llo
bat
ed
(s
m
oot
h)
Sm
ooth
to
p
bilo
ba
te
s
20
Recta
ngle
bilo
ba
te
s
Square
bilo
bate
s
20
Long
ce
lls
cle
ar
Long
cells
dark
Papill
aeEpid
er
m
al
ce
lls
w
avy
(thick)
Epid
erm
alstra
ig
ht(w
id
e)
Trichom
e
Arr
owArrow
ty
pe
butsm
oot
he
rto
p
and
1
si
de
lo
nger
20 40 60
C
ube
CuboidG
eom
etric
tr
ia
ng
le
U
nknow
n
2
ovalsh
ape
s
U
nknow
n
3
pla
ntshapes
epid
erm
a
lty
pes
lo
sts
ofci
rc
le
s
unlin
earsm
all
U
nknow
n
cle
arshapes
geo
m
etric
epid
erm
alce
lls
sm
all
cicle
s
non
linear
Bilo
bate
s
oth
er
D
ia
to
m
s
Epid
erm
alcells
la
rg
e
circle
s
unlin
ear
Epid
erm
alcel
ls
la
rg
e
circl
es
lin
ear
Sta
rsh
aped
phyt
olit
h
Snail
sh
ells
20 40
Charc
oaland
burn
tphyto
lit
hs
100 200 300
Tota
lP
hyto
lit
hs
Zon e
Zone 1
Zone 2
Zone 3
Forest Sedge and Grass Unidentified
Snails
Burnt
Casa Corona
Preliminary Phytolith results
0,2 0,4 0,6 0,8 1,0 1,2
Total sum o f squares
CONISS
Aims and Objectives
Main aims
 1) To examine the Palaeoenvironmental context of the Mesolithic-Neolithic
transition in Eastern Iberia
 To understand the effects of environmental stress on prehistoric communities.
 The anthropogenic impact of the first agricultural and husbandary systems on
landscape (7500-4000 cal BP)
Main objectives
 To use multi-proxy high resolution analysis
 to determine abrupt climatic/environmental events in the palaeoecological
record.
 and to compare these events with changes in human signatures during the
Mesolithic-Bronze age.
Yacimiento Cronología Distancia respecto
a los sondeos de
polen
Casa Corona Mesolítico Antiguo
Mesolítico Reciente
Neolítico
Campaniforme
Sondeo 4: 0 km
Sondeo 3: 5,4 km
Arenal de la
Virgen
Mesolítico Antiguo
Neolítico Antiguo
Sondeo 1: 0,5 km
Sondeo 2: 1,3 km
Sondeo 3
Pinar de Tarruella Epipaleolítico Sondeo 1: 0,6 km
Sondeo 2: 1,1 km
Sondeo 3: 1,1 km
Peñon de la Zorra Campaniforme Sondeo 4: 5,8 km
Sondeo 3: 8 km
Terlinques Edad del Bronce Sondeo 1: 2 km
Sondeo 3: 3,1 km
Cabezo Redondo Edad del Bronce Sondeo 4: 4,3 km
Sondeo 3: 3,2 km
El Castellar Fenicio (ss.VII-VI a.C.) Sondeo 1: 1 km
Sondeo 3: 1,7 km
Casas del Campo Romano Sondeo 4: 1,8 km
Sondeo 3: 5,6 km
Site Location
Figure 1:
Map showing the site locations
of Casa Corona and Villena lake
Table 1:
A list of archaeological sites within
close vicinity of the pollen core
sites soneo 1-4
Arenal de la Virgen (Villena lake)
 Mesolithic single occupation Phase
7750±40 BP, 8600-8430 Cal BP
 Excavations yielded: A partially
altered hearth structure; Burnt
sands; Fire cracked stones; Lithic
artefacts and Terrestrial gastropods
Pinar de Tarruella
(EPIPALEOLITHIC)
Pinar de Tarruella
(EPIPALEOLITHIC)Arenal de la Virgen
(MESOLITHIC and
EARLY NEOLITHIC
Arenal de la Virgen
(MESOLITHIC and
EARLY NEOLITHIC
Fig 2: Villena basin
site location
Fig 3: Notched and
Denticulated lithic
artefacts from
Arenal de la Vigen
Fig 4: Occupation phase at Arenal de
Vigen (2007)
Fig 5: Map of the
former Villena lake
Archaeology of the Villena basin i
Archaeology of the Villena basin ii
Casa Corona (Villena lake)
 Initial occupation during the Younger Dryas.
 Early Mesolithic phase: at least 2 hearths
 Late Mesolithic phase
 Neolithic find: 1 pit with Neolithic Post-Cardial
ceramic ware.
 The Chalcolithic phase: a settlement with pit
structures and ceramic sherds.
Fig 8: Excavation site before the railwayFig 7: Plan of excavation site
Fig 6: Core sampling for palaeoecological analysis,
after the railway, in April 2014
Fig 9: Mesolithic hearth with land snails
Archaeology of the Villena basin ii
Casa Corona (Villena lake)
 Late Mesolithic phase: at least one hearth, 2 pit
graves, trapezes, pierced shells, fauna remains
and rich land-snail deposits.Two Late Mesolithic
burials 8010-7800 cal BP.
 Isotope analysis=predominantly terrestrial
despite proximity to lake
Fig 10: Late Mesolithic burial at Casa Corona from Javier Fernandez et al., 2013
Rational for Palaeoecological Analysis
Climate has not remained stable-Abrupt 1500 yr events-The 8.2 event is one of the most
pronounced.
Despite wide acceptance of cooler and drier conditions recorded in the Mediterranean region
during Bond events:
It is still unclear how the Bond events have affected prehistoric cultures, particularly
Mesolithic mobility-strategies and the transition to agriculture.
A lack of high resolution palaeo-environmental
data from Late Mesolithic settlement areas
Weak chronologies or well dated lake cores
located far away from late Mesolithic sites
Chronology gaps in many records
Villena basin: Outstanding no. of
archaeological sites: Epipaleolithic- Bronze
age
35 km from the oldest documented Neolithic
sites & domesticated cereals
Archaeological record adjacent to environmental record
Continuous chronology spanning Epipaleolithic-Bronze age
Spans the Neolithic transition
More precise and thorough analysis on the effects of Bond events on prehistoric societies
Previous work:
•The Villena lake was investigated during the late 90`s, although accurate
pollen, biotic and sedimentary data are only available for the Late Glacial
and Early Holocene
•Pollen analysis:
Villena Lagoon (Yll et al., 2003, Fernández-López de Pablo et al., 2011):
•Villena: Stable isotope δ18O and δ13C analysis of land snails shell
carbonates from Mesolithic archaeological deposits (Yanes et al., 2013)
•Salinas Playa Lake (Giralt 1999, Giralt 2003, Julià 1996, Burjachs 2009)
Methods employed
Figs 11 & 12: Core samples extracted from Villena
lake VL3, 2014
Figs 13, 14 & 15: Core samples undergoing Magnetic Susceptibility from lake
VL3, 2014
Fig 16: Magnetic Susceptibility Scanner, Barcelona
An example of a small section of the results:
Palynomorphs, pollen and geochemical
Botryococcus Phytolith:Geometric
Type 119 (in
Van Geel)
Altenaria
Burnt stomata Chenopodiaceae
Pinus Burnt epidermal cells
Fig 18: Most common pollen and
palynomorphs from VL3
Fig 17: Aquatic Palynomorphs covering 7 m of VL3
Fig 20: Plantago (red) & Ericaceae (blue)
Fig 19: Charcoal (red) & Large Poaceae (blue)
Fig 21: Calcium (orange) and Olea (blue)
Concluding Comments
Current State of Investigation:
Multi-proxy analysis for the VL3 core has now been completed.
Interpretation of the data sets is now underway and the results will be submitted
for publishing before Feb 2016
Presentation of the results will be provided at the MEDINES conference 2016 in
Tarragona:
https://medinesworkshop2016.wordpress.com/
sjones@iphes.cat or sjones13@qub.ac.uk
Thank you
“PRETM”
Prehistoric Transitions in the Mediterranean: Cultural and economic responses to climate
change during the Mesolithic-Bronze Age
PEOPLE
MARIE CURIE ACTIONS
Intra-European Fellowships (IEF)
“POSTGLACIAL-MED”
Dinámica ambiental y respuestas humanas durante el Postglacial en la fachada mediterránea
de la Península Ibérica (c.12,700-8000 cal BP) (HAR 2013-41197)
“
Mediterranean Archaeological Landscapes: Postpalaeolithic adaptations, paleodemography
and land use patterns (RYC-2011-09363)

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Conference presentation Mesolithic Burgos

  • 1. Mesolithic to Bronze Age landscape signatures during periods of abrupt climate change: current work from the Upper Vinalopó Valley (SE Spain) lake deposits Marie-Curie Intra-European Fellowship: IEF-628589 Dr. Samantha E Jones; Prof. Fransesc B Casas; Dr. Javier Fernández- Lopez de Pablo 50 100 150 200 250 300 350 400 Depth D ecora te d fo re stty pes 20 Facet ate Fore stty pes Sedge pattern ed & w ithoutapic es Sedge bulli fo rm s w ith hor ns? G ra ss bullifo rm ssm ooth to p Pooid eae bilo ba te s H atbi lo bate s Tw o poi ntbi llo bat ed (s m oot h) Sm ooth to p bilo ba te s 20 Recta ngle bilo ba te s Square bilo bate s 20 Long ce lls cle ar Long cells dark Papill aeEpid er m al ce lls w avy (thick) Epid erm alstra ig ht(w id e) Trichom e Arr owArrow ty pe butsm oot he rto p and 1 si de lo nger 20 40 60 C ube CuboidG eom etric tr ia ng le U nknow n 2 ovalsh ape s U nknow n 3 pla ntshapes epid erm a lty pes lo sts ofci rc le s unlin earsm all U nknow n cle arshapes geo m etric epid erm alce lls sm all cicle s non linear Bilo bate s oth er D ia to m s Epid erm alcells la rg e circle s unlin ear Epid erm alcel ls la rg e circl es lin ear Sta rsh aped phyt olit h Snail sh ells 20 40 Charc oaland burn tphyto lit hs 100 200 300 Tota lP hyto lit hs Zon e Zone 1 Zone 2 Zone 3 Forest Sedge and Grass Unidentified Snails Burnt Casa Corona Preliminary Phytolith results 0,2 0,4 0,6 0,8 1,0 1,2 Total sum o f squares CONISS
  • 2. Aims and Objectives Main aims  1) To examine the Palaeoenvironmental context of the Mesolithic-Neolithic transition in Eastern Iberia  To understand the effects of environmental stress on prehistoric communities.  The anthropogenic impact of the first agricultural and husbandary systems on landscape (7500-4000 cal BP) Main objectives  To use multi-proxy high resolution analysis  to determine abrupt climatic/environmental events in the palaeoecological record.  and to compare these events with changes in human signatures during the Mesolithic-Bronze age.
  • 3. Yacimiento Cronología Distancia respecto a los sondeos de polen Casa Corona Mesolítico Antiguo Mesolítico Reciente Neolítico Campaniforme Sondeo 4: 0 km Sondeo 3: 5,4 km Arenal de la Virgen Mesolítico Antiguo Neolítico Antiguo Sondeo 1: 0,5 km Sondeo 2: 1,3 km Sondeo 3 Pinar de Tarruella Epipaleolítico Sondeo 1: 0,6 km Sondeo 2: 1,1 km Sondeo 3: 1,1 km Peñon de la Zorra Campaniforme Sondeo 4: 5,8 km Sondeo 3: 8 km Terlinques Edad del Bronce Sondeo 1: 2 km Sondeo 3: 3,1 km Cabezo Redondo Edad del Bronce Sondeo 4: 4,3 km Sondeo 3: 3,2 km El Castellar Fenicio (ss.VII-VI a.C.) Sondeo 1: 1 km Sondeo 3: 1,7 km Casas del Campo Romano Sondeo 4: 1,8 km Sondeo 3: 5,6 km Site Location Figure 1: Map showing the site locations of Casa Corona and Villena lake Table 1: A list of archaeological sites within close vicinity of the pollen core sites soneo 1-4
  • 4. Arenal de la Virgen (Villena lake)  Mesolithic single occupation Phase 7750±40 BP, 8600-8430 Cal BP  Excavations yielded: A partially altered hearth structure; Burnt sands; Fire cracked stones; Lithic artefacts and Terrestrial gastropods Pinar de Tarruella (EPIPALEOLITHIC) Pinar de Tarruella (EPIPALEOLITHIC)Arenal de la Virgen (MESOLITHIC and EARLY NEOLITHIC Arenal de la Virgen (MESOLITHIC and EARLY NEOLITHIC Fig 2: Villena basin site location Fig 3: Notched and Denticulated lithic artefacts from Arenal de la Vigen Fig 4: Occupation phase at Arenal de Vigen (2007) Fig 5: Map of the former Villena lake Archaeology of the Villena basin i
  • 5. Archaeology of the Villena basin ii Casa Corona (Villena lake)  Initial occupation during the Younger Dryas.  Early Mesolithic phase: at least 2 hearths  Late Mesolithic phase  Neolithic find: 1 pit with Neolithic Post-Cardial ceramic ware.  The Chalcolithic phase: a settlement with pit structures and ceramic sherds. Fig 8: Excavation site before the railwayFig 7: Plan of excavation site Fig 6: Core sampling for palaeoecological analysis, after the railway, in April 2014
  • 6. Fig 9: Mesolithic hearth with land snails Archaeology of the Villena basin ii Casa Corona (Villena lake)  Late Mesolithic phase: at least one hearth, 2 pit graves, trapezes, pierced shells, fauna remains and rich land-snail deposits.Two Late Mesolithic burials 8010-7800 cal BP.  Isotope analysis=predominantly terrestrial despite proximity to lake Fig 10: Late Mesolithic burial at Casa Corona from Javier Fernandez et al., 2013
  • 7. Rational for Palaeoecological Analysis Climate has not remained stable-Abrupt 1500 yr events-The 8.2 event is one of the most pronounced. Despite wide acceptance of cooler and drier conditions recorded in the Mediterranean region during Bond events: It is still unclear how the Bond events have affected prehistoric cultures, particularly Mesolithic mobility-strategies and the transition to agriculture. A lack of high resolution palaeo-environmental data from Late Mesolithic settlement areas Weak chronologies or well dated lake cores located far away from late Mesolithic sites Chronology gaps in many records Villena basin: Outstanding no. of archaeological sites: Epipaleolithic- Bronze age 35 km from the oldest documented Neolithic sites & domesticated cereals Archaeological record adjacent to environmental record Continuous chronology spanning Epipaleolithic-Bronze age Spans the Neolithic transition More precise and thorough analysis on the effects of Bond events on prehistoric societies
  • 8. Previous work: •The Villena lake was investigated during the late 90`s, although accurate pollen, biotic and sedimentary data are only available for the Late Glacial and Early Holocene •Pollen analysis: Villena Lagoon (Yll et al., 2003, Fernández-López de Pablo et al., 2011): •Villena: Stable isotope δ18O and δ13C analysis of land snails shell carbonates from Mesolithic archaeological deposits (Yanes et al., 2013) •Salinas Playa Lake (Giralt 1999, Giralt 2003, Julià 1996, Burjachs 2009)
  • 9. Methods employed Figs 11 & 12: Core samples extracted from Villena lake VL3, 2014 Figs 13, 14 & 15: Core samples undergoing Magnetic Susceptibility from lake VL3, 2014 Fig 16: Magnetic Susceptibility Scanner, Barcelona
  • 10. An example of a small section of the results: Palynomorphs, pollen and geochemical Botryococcus Phytolith:Geometric Type 119 (in Van Geel) Altenaria Burnt stomata Chenopodiaceae Pinus Burnt epidermal cells Fig 18: Most common pollen and palynomorphs from VL3 Fig 17: Aquatic Palynomorphs covering 7 m of VL3 Fig 20: Plantago (red) & Ericaceae (blue) Fig 19: Charcoal (red) & Large Poaceae (blue) Fig 21: Calcium (orange) and Olea (blue)
  • 11. Concluding Comments Current State of Investigation: Multi-proxy analysis for the VL3 core has now been completed. Interpretation of the data sets is now underway and the results will be submitted for publishing before Feb 2016 Presentation of the results will be provided at the MEDINES conference 2016 in Tarragona: https://medinesworkshop2016.wordpress.com/ sjones@iphes.cat or sjones13@qub.ac.uk Thank you
  • 12. “PRETM” Prehistoric Transitions in the Mediterranean: Cultural and economic responses to climate change during the Mesolithic-Bronze Age PEOPLE MARIE CURIE ACTIONS Intra-European Fellowships (IEF) “POSTGLACIAL-MED” Dinámica ambiental y respuestas humanas durante el Postglacial en la fachada mediterránea de la Península Ibérica (c.12,700-8000 cal BP) (HAR 2013-41197) “ Mediterranean Archaeological Landscapes: Postpalaeolithic adaptations, paleodemography and land use patterns (RYC-2011-09363)