1
Woodland use in the Montafon during Bronze Age Anton Stefan Schwarz 1 & Klaus Oeggl 1 Early Bronze Age charcoal spectrum Others 11% Deciduous 13% Pioneers 2% Coniferous 74% Literature: Krause R., 2006: Zur bronzezeitlichen Siedlungskammer im Montafon. Neue Ausgrabungen in Bartholomäberg. Bezirk Bludenz. Jahrbuch des Vorarlberger Landesmuseums 149, 47-60. Schmidl A., Kofler W., Oeggl-Wahlmüller N. & Oeggl K., 2005: Land use in the eastern Alps during the Bronze Age - An archaeobotanical case study of a hilltop settlement in the Montafon (Western Austria), Archaeometry (2005) 47, 2, 455-470. Schwarz A. S., Krause R., Oeggl K., (in press): Anthracological analysis from a mining site in the Eastern Alps to evaluate woodland uses during the Bronze Age. Proceedings of the 4th International Meeting of Anthracology, British Archaeological Reports International Series. 1 Innsbruck University, Institute of Botany, Sternwartestrasse 15, A-6020 Innsbruck, Austria; e-mail: [email protected] ; [email protected] Middle Bronze Age charcoal spectrum Others 3% Deciduous 2% Coniferous 65% Pioneers 30% Introduction In the Montafon (Vorarlberg, Austria) archaeological excavations (Fig.1) unearthed a fortified hilltop settlement ‘Friaga’ (Fig.2). The site was inhabited during the Early (19 th /18 th cent. BC), the Middle Bronze Age (16 th /15 th cent. BC) and the Iron Age (6 th /5 th cent. BC). Carbonised plant remains indicate a well developed Bronze Age husbandry regime. Previous palynological results from a nearby mire disclose large scale regional settlement activities during the Bronze Age (Schmidl et al., 2005). In the vicinity of the settlement ‘Friaga’ an additional dwelling place ‘Bodaweg’ (Fig.3) was occupied during the late Early (18 th /17 th cent. BC) and the younger Middle Bronze Age (14 th /13 th cent. BC). The cultural layers are concentrated in several pits (Fig.3) dispersed randomly over the excavation site. The analysis of the charcoal (Fig.4) enables an estimation of the use of wood in prehistory. Acknowledgements This study was carried out within the special research programme HiMAT ’The History of Mining Activities in the Tyrol and Adjacent Areas – Impact on Environment & Human Societies’ (www.uibk.ac.at/himat) funded by the Austrian National Science Fund FWF (grant nos: F3108, F3111), Land Vorarlberg, Stand Montafon and the communes Bartholomäberg and Silbertal. Tab.1: Other carbonised macro plant remains found from 18 charcoal-rich samples at the excavation site ‘Bodaweg’. Results and Discussion Charcoal analysis suggest an undisturbed mountain mixed forest (Abieti-Piceetum) in the surroundings of the settlement during the Early Bronze Age. Spruce (Picea/Larix type) is dominant, whereas beech (Fagus sylvatica), fir (Abies), maple (Acer) and lime (Tilia) are admixed. During Middle Bronze Age the occurrence of charcoal from pioneer species like birch (Betula), hazel (Corylus avellana), alder (Alnus) and rowan (Sorbus) reflects an extensive opening of the forest. All timber had mean diameters <10cm (Tab.2) and was in most cases 11 to 40 years old (Fig.5). These indicate burning of branches and twigs as well as young trees. The constant gathering of timber from Early Bronze Age onwards led to a retreat of the natural climax wood. Consequently, the Middle Bronze Age pits reveal high amounts of fast growing and light demanding pioneer species (Fig.6 and Fig.7). Deciduous wood derives mainly from hedges or coppices admixed with a few branches from adult trees, e.g. beech (Fagus sylvatica) or maple (Acer). Coniferous wood is still mainly composed by branches and twigs from adult trees resulting in ongoing forest opening e.g. for pasturing (Schwarz et al., in press). Palynological records (Fig.8) of the nearby mire ‘Tschuga’ reaffirm an immense Bronze Age clearing by a sudden decrease of spruce (Picea) and fir (Abies) associated with an increase of grasses (Gramineae) in the pollen diagram (Schmidl et al., 2005). The anthropogenic impact is well documented by the frequent presence of cultural and pastoral indicators together with the increase of micro charcoal particles, particularly during the Middle Bronze Age. Fig.8: Simplified pollen percentage diagram of the mire at Tschuga. EBA = Early Bronze Age, MBA = Middle Bronze Age, LBA = Late Bronze Age, IA = Iron Age, RA = Roman Age, MA = Middle Ages, MT = Modern Times (Schmidl et al. 2005). Conclusion The charcoal analysis reflects the anthropogenic change of the local woodland over time. The Early Bronze Age mountain mixed forest (Fig.9) shifted into a more open spruce (Picea)-dominated mixed forest with high values of pioneers (Fig.10) in the Middle Bronze Age, indicating a consistent anthropogenic opening of the forest. In addition, palynological studies from a nearby mire reaffirm a high demand on farming land and timber during Bronze Age. Fig.5: The calculated age classes a) of the deciduous and b) the coniferous wood suggest the burning of branches and twigs from adult trees and wood from a coppice or hedge. The age was calculated by dividing the radius of the piece by the mean ring width. Tab.2: Results of the charcoal analysis presented in percentage values from the excavation site ‘Bodaweg’. The pits are ordered chronological. Species ordered following ecological dispersal. If possible, the radius of the charcoal pieces was measured and the mean diameter (mD) was calculated from coniferous as well from deciduous wood for each sample. Fig.6: Pits ordered in case of a Principle Component Analysis of the percent values (%) of charred species. Same types of pits cluster together. The difference between Early Bronze Age pits and Middle Bronze Age pits is obvious. Furthermore differ the two types of pits from the Middle Bronze Age in their charcoal composition. Yellow: Middle Bronze Age ‘type b’ pit; green: Middle Bronze Age ‘type a’ pit; blue: Early Bronze Age ‘type eba’ pit. Fig.7: The Principle Component Analysis of the percent values (%) of the used species in detail. The direction and length of the arrows indicate the influence of the species for position of the sample in the diagram. Positive correlating arrows point to the same direction, while negative correlating species show opposite directions. Yellow: Middle Bronze Age ‘type b’ pit; green: Middle Bronze Age ‘type a’ pit; blue: Early Bronze Age ‘type eba’ pit. Fig.10: Composition of the Middle Bronze Age wood (n=1000). Fig.9: Composition of the Early Bronze Age wood (n=375). Fig.3: The Bronze Age dwelling place ‘Bodaweg’: a) The cultural layers are concentrated in several pits. b) The pits are dispersed randomly over the site (geomagnetical surveys, see Krause R., 2006). Fig.4: Charcoal-rich layer from a pit (diameter = 2m, depth = 0,5m) at the excavation site ‘Bodaweg’. (Krause R., unpubl.). Fig.2: The Bronze Age fortified hilltop settlement ‘Friaga’ (Krause R., 2006): a) 3D-model by Martin Schaich, ArcTron Dokumentation, Altenthann b) Occupation layers. Fig.1: Investigation area in the Montafon (Bartholomäberg, Vorarlberg, Austria). Excavation site 1: The Bronze Age hilltop settlement ‘Friaga’ (940m a.s.l.) and site 2: The Bronze Age dwelling place ‘Bodaweg’ (980m a.s.l.), with the nearby mire ‘Tschuga’ (1200m a.s.l.). Several copper ore deposits are located at Bartholomäberg and Silbertal (Krause R., 2006 modified). Middle Bronze Age 16th/15th century BC Iron Age 5th/4th century BC Early Bronze Age 19th/18th century BC Middle Bronze Age 14th/13th century BC Early Bronze Age 18th/17th century BC Material and Methods 18 soil samples were systematically collected from the site ‘Bodaweg’ with a standardized volume (10 litres; see details in Tab.1). Carbonised plant remains were extracted using standard flotation technique. Approximately 100 charcoal pieces were randomly collected and analysed from each sample (Tab.2). a b a b Spruce (Picea) Fir (Abies) Tschuga Age of the burned deciduous wood 0% 10% 20% 30% 40% 50% 10 11-20 21-40 41-60 61-80 81-100 >100 n.s. age class [years] MBA 'type b' filled pits MBA 'type a' settlement pits EBA 'eba' pits Age of the burned coniferous wood 0% 10% 20% 30% 40% 50% 10 11-20 21-40 41-60 61-80 81-100 >100 n.s. age class [years] MBA 'type b' filled pits MBA 'type a' settlement pits EBA 'eba' pits b a Bartholomäberg Bodaweg Sample volume [l] Sample number Picea/Larix cf. Abies Fagus sylvatica Acer sp. Quercus sp. Tilia sp. Pinus sylvestris Corylus avellana Alnus sp. Betula sp. Betulaceae indet. Maloideae indet. cf. Clematis cf. Euonymus Pinaceae indet. Deciduous indet. indet. Total charcoal weight >2mm [g] Analysed charcoal weight >2mm [g] Analysed charcoal pieces Deciduous N mD Deciduous mD [cm] Coniferous N mD Coniferous mD [cm] MBA type 'b' 10 1 78 · · · · · · 20 · · · · · · · 2 · 20,6 3,1 50 11 5,77 39 6,01 MBA type 'b' * 10 7 90 · · · · · · 10 · · · · · · · · · 41,1 4,1 50 5 4,40 45 6,33 MBA type 'b' 10 11 74 · · 1 · · 2 14 · · 3 · · · 2 4 · 5,0 2,0 100 19 4,32 73 4,32 MBA type 'b' 10 16 65 · · · · · 1 21 6 7 · · · · · · · 104,1 16,1 100 34 4,41 66 5,48 MBA type 'b' 10 18 39 · · 3 2 · · 39 · 8 · 9 · · · · · 19,1 4,7 100 61 5,84 39 6,08 MBA type 'b' 10 23 51 · · · · · · 24 22 · · 3 · · · · · 19,7 6,7 100 49 4,98 51 5,73 MBA type 'b' 10 24 50 · · · · · 4 20 25 1 · · · · · · · 95,5 11,9 100 46 7,30 54 7,66 MBA type 'b' 10 28 58 · · · · · 2 29 9 · · · · · · 2 · 61,0 5,3 100 40 6,66 60 6,64 MBA type 'a' * 10 2 84 3 9 · · · 2 · · · · · · · 1 1 · 20,2 3,5 100 10 4,95 90 5,53 MBA type 'a' 10 4 83 · · · · · · · 6 7 2 · · · · 2 · 50,1 5,5 100 17 4,88 83 3,99 MBA type 'a' 10 12 59 · 3 · · · · 10 · 3 1 9 · · 5 10 · 2,2 1,6 100 33 2,80 61 2,98 EBA type 'eba' 10 8 89 · 2 4 · · · · · · · · · · · 2 3 40,4 7,3 100 6 4,33 87 6,49 EBA type 'eba' 10 9 81 2 4 4 · · · · · · · · · · 1 8 · 15,8 4,9 100 12 5,54 81 5,97 EBA type 'eba' 10 10 59 10 6 · · · 1 · · · · 3 · 1 19 1 · 5,3 3,1 100 9 5,11 86 5,16 EBA type 'eba' 10 13 56 8 28 · · 8 · · · · · · · · · · · 2,6 0,8 25 9 5,83 16 5,13 EBA type 'eba' 5 39 46 · 34 2 · · · 4 · · · 2 4 · · 8 · 4,9 3,7 50 27 5,46 23 6,33 [%] Sum 155 all 507,6 84,3 1375 388 5,37 954 5,52 EBA Early Bronze Age type 'eba' pits N Number * 1 of 2 samples MBAMiddle Bronze Age type 'a' settlement pit type 'b' filled pit mD mean Diameter mountain mixed forest pioneers others Bartholomäberg Bodaweg Bronze Age Period Early Middle Middle Type of pit type 'eba' type 'a' type 'b' Samples 5 4 9 Sample volume [l] 45 40 90 Cereals Hordeum vulgare · 2 6 Hordeum sp. · · 2 Cerealia indet. · · 1 Triticum spelta (spikelet fork) · · 1 Gathered plants Prunus spinosa · 1 · Rubus idaeus 11 3 · Sambucus nigra 1 2 1 Sambucus sp. · 1 · Wild plants Avena sp. (awn fragment) · · 1 Chenopodium sp. · 3 · Fabaceae 1 · · Galium sp. · 1 · Polygonum aviculare · · 1 Silene sp. 1 · · Solanum nigrum 1 · · Spergularia sp. · · 1 Woodland Picea abies (needle fragment) · 1 · Bronze Age Identified charred plant remains Diaspores and (others)

Anton Stefan Schwarz - Universität Innsbruck · 2019. 4. 2. · Woodland use in the Montafon during Bronze Age Anton Stefan Schwarz 1 & Klaus Oeggl 1 Early Bronze Age charcoal spectrum

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Page 1: Anton Stefan Schwarz - Universität Innsbruck · 2019. 4. 2. · Woodland use in the Montafon during Bronze Age Anton Stefan Schwarz 1 & Klaus Oeggl 1 Early Bronze Age charcoal spectrum

Woodland use in the Montafon during Bronze AgeAnton Stefan Schwarz1 & Klaus Oeggl1

Early Bronze Agecharcoal spectrum

Others11%

Deciduous13%Pioneers

2%

Coniferous74%

Literature:Krause R., 2006: Zur bronzezeitlichen Siedlungskammer im Montafon. Neue Ausgrabungen in Bartholomäberg. Bezirk Bludenz. Jahrbuch des Vorarlberger Landesmuseums 149, 47-60.Schmidl A., Kofler W., Oeggl-Wahlmüller N. & Oeggl K., 2005: Land use in the eastern Alps during the Bronze Age - An archaeobotanical case study of a hilltop settlement in the Montafon (Western Austria), Archaeometry (2005) 47, 2, 455-470.Schwarz A. S., Krause R., Oeggl K., (in press): Anthracological analysis from a mining site in the Eastern Alps to evaluate woodland uses during the Bronze Age. Proceedings of the 4th International Meeting of Anthracology, British Archaeological Reports International Series.1 Innsbruck University, Institute of Botany, Sternwartestrasse 15, A-6020 Innsbruck, Austria; e-mail: [email protected]; [email protected]

Middle Bronze Agecharcoal spectrum

Others3%

Deciduous2%

Coniferous65%

Pioneers30%

IntroductionIn the Montafon (Vorarlberg, Austria) archaeological excavations (Fig.1) unearthed a fortified hilltop settlement ‘Friaga’ (Fig.2). The site was inhabited during the Early (19th/18th cent. BC), the Middle Bronze Age (16th/15th cent. BC) and the Iron Age (6th/5th cent. BC). Carbonised plant remains indicate a well developed Bronze Age husbandry regime. Previous palynological results from a nearby mire disclose large scale regional settlement activities during the Bronze Age (Schmidl et al., 2005). In the vicinity of the settlement ‘Friaga’ an additional dwelling place ‘Bodaweg’(Fig.3) was occupied during the late Early (18th/17th cent. BC) and the younger Middle Bronze Age (14th/13th cent. BC). The cultural layers are concentrated in several pits (Fig.3) dispersed randomly over the excavation site. The analysis of the charcoal (Fig.4) enables an estimation of the use of wood in prehistory.

AcknowledgementsThis study was carried out within the special research programme HiMAT’The History of Mining Activities in the Tyrol and Adjacent Areas – Impact on Environment & Human Societies’ (www.uibk.ac.at/himat) funded by the Austrian National Science Fund FWF (grant nos: F3108, F3111), Land Vorarlberg, Stand Montafon and the communes Bartholomäberg and Silbertal.

Tab.1: Other carbonised macro plant remains found from 18 charcoal-rich samples at the excavation site ‘Bodaweg’.

Results and DiscussionCharcoal analysis suggest an undisturbed mountain mixed forest (Abieti-Piceetum) in the surroundings of the settlement during the Early Bronze Age. Spruce (Picea/Larix type) is dominant, whereas beech (Fagussylvatica), fir (Abies), maple (Acer) and lime (Tilia) are admixed. During Middle Bronze Age the occurrence of charcoal from pioneer species like birch (Betula), hazel (Corylus avellana), alder (Alnus) and rowan (Sorbus) reflects an extensive opening of the forest.All timber had mean diameters <10cm (Tab.2) and was in most cases 11 to 40 years old (Fig.5). These indicate burning of branches and twigs as well as young trees. The constant gathering of timber from Early Bronze Age onwards led to a retreat of the natural climax wood.Consequently, the Middle Bronze Age pits reveal high amounts of fast growing and light demanding pioneer species (Fig.6 and Fig.7). Deciduous wood derives mainly from hedges or coppices admixed with a few branches from adult trees, e.g. beech (Fagus sylvatica) or maple (Acer). Coniferous wood is still mainly composed by branches and twigs from adult trees resulting in ongoing forest opening e.g. for pasturing (Schwarz et al., in press). Palynological records (Fig.8) of the nearby mire ‘Tschuga’ reaffirm an immense Bronze Age clearing by a sudden decrease of spruce (Picea) and fir (Abies) associated with an increase of grasses (Gramineae) in the pollen diagram (Schmidl et al., 2005). The anthropogenic impact is well documented by the frequent presence of cultural and pastoral indicators together with the increase of micro charcoal particles, particularly during the Middle Bronze Age.

Fig.8: Simplified pollen percentage diagram of the mire at Tschuga. EBA = Early Bronze Age, MBA = Middle Bronze Age, LBA = Late Bronze Age, IA = Iron Age, RA = Roman Age, MA = Middle Ages, MT = Modern Times (Schmidl et al. 2005).

ConclusionThe charcoal analysis reflects the anthropogenic change of the local woodland over time. The Early Bronze Age mountain mixed forest (Fig.9) shifted into a more open spruce (Picea)-dominated mixed forest with high values of pioneers (Fig.10) in the Middle Bronze Age, indicating a consistent anthropogenic opening of the forest. In addition, palynological studies from a nearby mire reaffirm a high demand on farming land and timber during Bronze Age.

Fig.5: The calculated age classes a) of the deciduous and b) the coniferous wood suggest the burning of branches and twigs from adult trees and wood from a coppice or hedge. The age was calculated by dividing the radius of the piece by the mean ring width.

Tab.2: Results of the charcoal analysis presented in percentage values from the excavation site ‘Bodaweg’. The pits are ordered chronological. Species ordered following ecological dispersal. If possible, the radius of the charcoal pieces was measured and the mean diameter (mD) was calculated from coniferous as well from deciduous wood for each sample.

Fig.6: Pits ordered in case of a Principle Component Analysis of the percent values (√%) of charred species. Same types of pits cluster together. The difference between Early Bronze Age pits and Middle Bronze Age pits is obvious. Furthermore differ the two types of pits from the Middle Bronze Age in their charcoal composition.Yellow: Middle Bronze Age ‘type b’ pit; green: Middle Bronze Age ‘type a’ pit; blue: Early Bronze Age ‘type eba’ pit.

Fig.7: The Principle Component Analysis of the percent values (√%) of the usedspecies in detail. The direction and length of the arrows indicate the influence of the species for position of the sample in the diagram. Positive correlating arrows point to the same direction, while negative correlating species show opposite directions.Yellow: Middle Bronze Age ‘type b’ pit; green: Middle Bronze Age ‘type a’ pit; blue: Early Bronze Age ‘type eba’ pit.

Fig.10: Composition of the Middle Bronze Age wood (n=1000).

Fig.9: Composition of the Early Bronze Age wood (n=375).

Fig.3: The Bronze Age dwelling place ‘Bodaweg’:a) The cultural layers are concentrated in several pits.b) The pits are dispersed randomly over the site (geomagnetical surveys, see Krause R., 2006).

Fig.4: Charcoal-rich layer from a pit (diameter = 2m, depth = 0,5m) at the excavation site ‘Bodaweg’. (Krause R., unpubl.).

Fig.2: The Bronze Age fortified hilltop settlement ‘Friaga’ (Krause R., 2006):a) 3D-model by Martin Schaich, ArcTron Dokumentation, Altenthannb) Occupation layers.

Fig.1: Investigation area in the Montafon (Bartholomäberg, Vorarlberg, Austria).Excavation site 1: The Bronze Age hilltop settlement ‘Friaga’ (940m a.s.l.)and site 2: The Bronze Age dwelling place ‘Bodaweg’ (980m a.s.l.),with the nearby mire ‘Tschuga’ (1200m a.s.l.). Several copper ore deposits are located at Bartholomäberg and Silbertal (Krause R., 2006 modified).

Middle Bronze Age 16th/15th

century BC

Iron Age 5th/4th

century BC

Early Bronze Age 19th/18th

century BC

Middle Bronze Age 14th/13th

century BC

Early Bronze Age 18th/17th

century BC

Material and Methods18 soil samples were systematically collected from the site ‘Bodaweg’ with a standardized volume (10 litres; see details in Tab.1). Carbonised plant remains were extracted using standard flotation technique. Approximately 100 charcoal pieces were randomly collected and analysed from each sample (Tab.2).

a b

a b

Spruce

(Picea)

Fir

(Abies)

Tschuga

Age of the burned deciduous wood

0%

10%

20%

30%

40%

50%

≤10 11-20 21-40 41-60 61-80 81-100 >100 n.s.

age class [years]

MBA 'type b' filled pits MBA 'type a' settlement pits EBA 'eba' pits

Age of the burned coniferous wood

0%

10%

20%

30%

40%

50%

≤10 11-20 21-40 41-60 61-80 81-100 >100 n.s.

age class [years]

MBA 'type b' filled pits MBA 'type a' settlement pits EBA 'eba' pits

ba

Bar

thol

omäb

erg

Bod

aweg

Sam

ple

volu

me

[l]

Sam

ple

num

ber

Pic

ea/L

arix

cf. A

bies

Fag

us s

ylva

tica

Ace

r sp

.

Que

rcus

sp.

Tili

a sp

.

Pin

us s

ylve

stris

Cor

ylus

ave

llana

Aln

us s

p.

Bet

ula

sp.

Bet

ulac

eae

inde

t.

Mal

oide

ae in

det.

cf. C

lem

atis

cf. E

uony

mus

Pin

acea

e in

det.

Dec

iduo

us in

det.

inde

t.

Tot

al c

harc

oal

wei

ght >

2mm

[g]

Ana

lyse

d ch

arco

alw

eigh

t >2m

m [g

]

Ana

lyse

d ch

arco

alpi

eces

Dec

iduo

usN

mD

Dec

iduo

usm

D [c

m]

Con

ifero

usN

mD

Con

ifero

usm

D [c

m]

MBA type 'b' 10 1 78 · · · · · · 20 · · · · · · · 2 · 20,6 3,1 50 11 5,77 39 6,01MBA type 'b' * 10 7 90 · · · · · · 10 · · · · · · · · · 41,1 4,1 50 5 4,40 45 6,33MBA type 'b' 10 11 74 · · 1 · · 2 14 · · 3 · · · 2 4 · 5,0 2,0 100 19 4,32 73 4,32MBA type 'b' 10 16 65 · · · · · 1 21 6 7 · · · · · · · 104,1 16,1 100 34 4,41 66 5,48MBA type 'b' 10 18 39 · · 3 2 · · 39 · 8 · 9 · · · · · 19,1 4,7 100 61 5,84 39 6,08MBA type 'b' 10 23 51 · · · · · · 24 22 · · 3 · · · · · 19,7 6,7 100 49 4,98 51 5,73MBA type 'b' 10 24 50 · · · · · 4 20 25 1 · · · · · · · 95,5 11,9 100 46 7,30 54 7,66MBA type 'b' 10 28 58 · · · · · 2 29 9 · · · · · · 2 · 61,0 5,3 100 40 6,66 60 6,64

MBA type 'a' * 10 2 84 3 9 · · · 2 · · · · · · · 1 1 · 20,2 3,5 100 10 4,95 90 5,53MBA type 'a' 10 4 83 · · · · · · · 6 7 2 · · · · 2 · 50,1 5,5 100 17 4,88 83 3,99MBA type 'a' 10 12 59 · 3 · · · · 10 · 3 1 9 · · 5 10 · 2,2 1,6 100 33 2,80 61 2,98

EBA type 'eba' 10 8 89 · 2 4 · · · · · · · · · · · 2 3 40,4 7,3 100 6 4,33 87 6,49EBA type 'eba' 10 9 81 2 4 4 · · · · · · · · · · 1 8 · 15,8 4,9 100 12 5,54 81 5,97EBA type 'eba' 10 10 59 10 6 · · · 1 · · · · 3 · 1 19 1 · 5,3 3,1 100 9 5,11 86 5,16EBA type 'eba' 10 13 56 8 28 · · 8 · · · · · · · · · · · 2,6 0,8 25 9 5,83 16 5,13EBA type 'eba' 5 39 46 · 34 2 · · · 4 · · · 2 4 · · 8 · 4,9 3,7 50 27 5,46 23 6,33

[%]

Sum 155 all 507,6 84,3 1375 388 5,37 954 5,52

EBA Early Bronze Age type 'eba' pits N Number * 1 of 2 samples MBA Middle Bronze Age type 'a' settlement pit type 'b' filled pit mD mean Diameter

mountain mixed forest pioneers others

Bartholomäberg BodawegBronze Age Period Early Middle MiddleType of pit type 'eba' type 'a' type 'b'Samples 5 4 9Sample volume [l] 45 40 90

CerealsHordeum vulgare · 2 6Hordeum sp. · · 2Cerealia indet. · · 1Triticum spelta (spikelet fork) · · 1

Gathered plantsPrunus spinosa · 1 ·

Rubus idaeus 11 3 ·

Sambucus nigra 1 2 1Sambucus sp. · 1 ·

Wild plantsAvena sp. (awn fragment) · · 1Chenopodium sp. · 3 ·

Fabaceae 1 · ·

Galium sp. · 1 ·

Polygonum aviculare · · 1Silene sp. 1 · ·

Solanum nigrum 1 · ·

Spergularia sp. · · 1Woodland

Picea abies (needle fragment) · 1 ·

Bronze Age

Identified charred plant remainsDiaspores and (others)