30012018 Flashcards

1
Q

Understanding Human-Environment Interaction In Ancient Mongolia

A
  • Lisa Jazz
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2
Q

Mongolia

A
  • Btw Russian Federation and People’s Republic of China
  • Climate: harsh extreme (-40 in winter to 100 in summer)
    > Dramatic change
  • Population: 10 years ago 30% lives in cities > increase now
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3
Q

Agriculturalists, herders, and hunter-gatherers in East Asia

A
  • Nomadic Pastoralists (beginning 3300 BC)
    • Moving settlements seasonally (1-2 times / yr)
    • Domesticated wheat + barley
    • Domesticated cattle, sheep, goats, horses
    • Milk + milk products
    • Wild sheep, goats, gazelle, deer, rabbits, birds, fish
    • Wild fruits, nuts, grains + tubers
  • Gobi Desert Hunter-Gatherers (until 1500 BC)
    • Moving settlements regularly
    • Wild horses, cattle, deer, sheep, goats, gazelle
    • Wild rabbits, birds, frogs ?
    • Wild greens, fruits, nuts, grains + tubers
    • Wild grass seeds
  • Agriculturalists (beginning 6000BC)
    • Large settlements in 1 place
    • Domesticated millet + rice
    • Domesticated pigs + chicken
    • Wild cattle, gazelle, deer, rabbits, birds, fish
    • Wild fruits, nuts, grains + tubers
      > Know the environment > Diet choice + eating habit
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4
Q

Gobi-Steppe Neolithic Project

A
  • Excavation include: burials, habitation sites

- Aim: how human adapt to environment change + how human change the environment as well

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5
Q

Mongolian Neolithic

A

Period | Dates | Tech | Land-use
Oasis 1 | 11500-6000BC | Pottery after 7700BC, microblades | High residential mobility, increasing use of wetlands
Oasis 2 | 6000-3000BC | Pottery, Microblades, grinding stones | Wetland-centric, logistic mobility
Oasis 3 / Bronze Age | 3000-1000BC | Pottery, microblades, bifaces, polished axes | Wetland-centric, mixed mobility?

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6
Q

Pleistocence (Ice Age) Ecosystems

A
  • 2.5 million to 11700 years ago
  • Fluctuation of climate since 120,000 years ago
  • Mammoth, giant beaver, Irish elk
  • Africa: covered by grassland > human = part of the grasslands (in the ecosystem)
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7
Q

Holocene (Post-Glacial) Ecosystems

A
  • 11700 years ago to present
  • Wetlands
    > Change types of food ppl ate
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8
Q

Human environmental impacts

A
  1. Wild fire
  2. Harvesting (e.g. wild rice)
  3. Human produce garbage for raccoons to eat
  4. Landscape engineering: the intentional way human modifying lands
    (E.g. coastal California landscapes were created by fire to suit the needs of indigenous hunter-gatherers; Australian indigenous gps use fire to improve environmental carrying capacity)
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9
Q

Anthropogenic (human modified) Landscapes

A

-

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10
Q

Human and landscape palaeoecology

A

3 important methods:

  1. Geoarchaeology
  2. Species identification
  3. Ecological modeling
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11
Q

Geoarchaeology

A
  1. Stratigraphy and soil types (e.g. river cut, wet-dry cycles)
  2. Dating sediments
  3. Microbotanical remains
  4. Mapping landforms
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12
Q

Zooarchaeology and Palaeoethnobotany

A
  1. Species (taxonomic) list (e.g. hare bones, grass seeds)
  2. Species identification
  3. Taphonomy
  4. Weights and counts
    - In dry cave, only burned seeds can survive
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13
Q

GIS-Based Ecological Modelling

A
  1. Compiling NASA satellite imagery
  2. Creating GIS-based hydrological models
  3. Modelling species interactions (community ecology)
  4. Modelling species distributions (MaxEnt)
  5. Refining models based on field tests
  6. Mapping on archaeological data
    * Many of them based on hydrology
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14
Q

Site: Zaraa Uul

A
- Getting bones in this landscape
> Hunting animals that are extinct today
> Suggest the environment is different
> Wetlands + grasslands > grasslands
> ? Former lake basin at Zaraa Uul > compared to HUla wetlands in Israel
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15
Q

Lecture

A

-

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16
Q

***Site formation (VERY IMPORTANT!!)

A
= Product of:
1. Material deposited:
  A. Type of material
  B. Process of deposition
       - accidental, e.g. loss
       - intentional, e.g. burial or trash
2. Environment
  A. Climatic variables
       - Acidic, e.g. NE Woodlands
       - Arid, e.g. American SW; highland Andes
       - Wet, e.g. Submerged, frozen
  B. Depositional setting
17
Q

Depositional environments

A
  1. Non-depositional (e.g. lakeshore)
  2. “Accretions” (e.g. rockshelter)
  3. Alluvial (e.g. floodplain)
18
Q
  1. Non-deposition environment
A

Non-depositional (e.g. lakeshore)
E.g. typical non-depositional sole profile
- “O” horizon 0-5cm below ground surface = zone of organic (dark)
- “A” horizon 5-15cm = zone of leaching, organic breakdown
- “B” horizon 15-38cm = zone of accumulation, chemical alteration
> Iron ores (Colors)
- “C” horizon >38cm = zone of inactive sediment, “parent material”
> Most of the things wont get burial in depth > close to surface
> <10% artifact distribution 40cm below the ground surface
- Fire-cracked rock: heat up the rocks > put into water > rocks crack > disposal
- Postholes > how ppl are organized

19
Q
  1. Accretional
A

Accretional (e.g. rockshelter)

- Little separation btw occupation

20
Q
  1. Alluvial
A

Alluvial (e.g. floodplain)
- Winooski - Burlington bridge @1928 taken by a flood
- Anthropogenic: generally made by human / human activities
> e.g. dark lines in btw light soils layers > human activities
- Site: Milo, Maine, perfect floodplain per 5 hundred years
- Better preservation: preserved by sand layers
- Site Howe Farm, Winooski River Intervale: Logs down > erosion