Title: Vegetation Change
1- Vegetation Change
- Environmental and Anthropogenic Controls on
Vegetation - Documenting Past Vegetation Changes
- A) Pollen
- B) Plant Macrofossils
- III) Paleovegetation Changes in Eastern North
America
2I) Environmental Controls
Terrestrial Ecosystems
Aquatic Life Zones
Sunlight Temperature Precipitation Wind
Latitude Altitude Fire frequency Soil
Light penetration Water currents Dissolved
nutrient concentrations (especially N and P)
Suspended solids
3Biotic - Range of Tolerance
(c)
(c)
(a)
(a)
(b)
4Forest Composition 1800 as Interpreted from GLO
Survey Notes by MNIF
5Community
6Plant succession
climax
Southeastern USA
7I) Environmental Controls B) Disturbance
8Photos from Michigan EPIC
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10Cahokia
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12Cahokia
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14- Vegetation Change
- Environmental and Anthropogenic Controls on
Vegetation - Documenting Past Vegetation Changes
- A) Pollen
- B) Plant Macrofossils
- III) Paleovegetation Changes in Eastern North
America
15- II) Past Vegetation Changes
- Pollen (Spores) Palynology
- 1. What are pollen spores?
16II) A) Pollen (Spores) 1. What are pollen
spores?
male cone (pollen)
Gymnosperms
female cone (seeds)
17Gymnosperms naked seeds
18Angiosperms
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22II) A) Pollen (Spores) 2. Pollen
Production, Dispersal Preservation
23- A)
- 2. Pollen Production, Dispersal Preservation
a) Size
Artemisia (sage( 40 µm)
Poaceae (grass) 60-100 µm
24 2. Pollen Production, Dispersal Preservation
a) Morphology gt Identification
- Variations in
- pores
- furrows
- sculpture
25Epilobium (fireweed)
26Sculpturing elements
tectum
columella
footwall
2710X
Objectives 20, 40, 100X
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292. Pollen Production, Dispersal Preservation
b) Pollen Production Dispersal
Anemophilous pollen
302. Pollen Production, Dispersal Preservation
b) Pollen Production Dispersal
(i) anemophilous wind-dispersed all conifers
Pinus (pine) Picea (spruce) Larix (tamarack)
Tsuga (hemlock) Carya (hickory) Betula
(birch) Quercus (oak) Populus (poplar)
variability in production Alnus (alder)
highest Pinus (pine) 2nd highest Fagus (beech)
least
31- (i) wind-dispersed anemophilous
- Herbs
- Poaceae (grass)
- Artemisia (sage, wormwood)
- Ambrosia-type (ragweed)
322. Pollen Production, Dispersal Preservation
b) Pollen Production Dispersal
(ii) insect-dispersed entomophilous
Malva (mallow)
Trees Acer (maple) Tilia (basswood)
33Lilium (lily)
Epilobium (fireweed)
342. Pollen Production, Dispersal Preservation
b) Pollen Production Dispersal
- (iii) AP/NAP
- Trees AP arboreal pollen
- Herbs NAP non-arboreal pollen
352. Pollen Production, Dispersal Preservation
c) Pollen Rain
- dispersed by air currents
- within canopy local (lt 20 m)
- extralocal, regional
- transported by water
- select lakes without inlets
Taphonomy
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37Big Stone Lake, MN
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40bioturbation
Moore et al. (1989)
412. Pollen Production, Dispersal Preservation
d) Pollen Preservation
Populus (poplar)
Picea (spruce)
422. e) Pollen Interpretation
0
Analyst Eric C. Grimm
43Coldwater Lake, ND Mid-Holocene Aridity
44- Vegetation Change
- Environmental and Anthropogenic Controls on
Vegetation - Documenting Past Vegetation Changes
- A) Pollen
- B) Plant Macrofossils
- III) Paleovegetation Changes in eastern North
America
45Proxies of Paleovegetation
POLLEN
PLANT MACROFOSSILS
Picea glauca (white spruce) seed
Picea (spruce) pollen
1 cm
20 ?m
macroscopic low abundance local
vegetation identify to species level
46B) Plant Macrofossils 1. Size
500 µm
Najas flexilis Chenopodium
berlandieri
47B) Plant Macrofossils
- 2. Species Identification
Hippuris vulgaris (mares- Tail)
48B) Plant Macrofossils 3. Production, Dispersal
Preservation
49- Vegetation Change
- Environmental and Anthropogenic Controls on
Vegetation - Documenting Past Vegetation Changes
- A) Pollen
- B) Plant Macrofossils
- III) Paleovegetation Changes in Eastern North
America
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51Miner Lake, Allegan Co., Michigan Core
Stratigraphy
52Individualistic Plant Migration
Picea migration northwards (green is 20 or
higher amounts of spruce pollen)
- 18 15 12 9
6 3 0 - ka (1000 yr
B.P.)
http//www.geo.brown.edu/georesearch/esh/QE/QEHome
.html
53Non-Analog Vegetation
14 ka 13 ka 12 ka 11 ka
10 ka
Calendar years Shuman et al. (2002)
540
Analyst Eric C. Grimm
55Refugia
5628,000 25,000 14C yr BP
57Reconstruction by R. Webb J. Overpeck for the
eastern USA.
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590
Fox River Stone Company Quarry, IL
60Dryas integrifolia (arctic dryad)
1 mm
61Floods -gt leaves other plant remains deposited
in proglacial lakes
Aktineq Glacier Bylot Island Nuvanut, Canada
Photo B. Shilts
62Illinois at 16,000 yr B.P.
http//www.museum.state.il.us/exhibits/larson/envi
ronments.html
63Late-Glacial Spruce Parkland
Yansa (2006)
6413,000 14C yr BP
65Changes in climate boundary conditions since the
Last Glacial Maximum
66Adapted from Overstreet (2002)
67Schaeffer Mammoth Site (1992-93)
Drainage tile (1964)
75 of skeleton intact adult male 36 years old
68Paleobotany of the Schaefer Site Core (2004)
Sources Stuiver et al. (1995) Cross (2002)
69Forming the Great Lakes
70Reconstruction by R. Webb J. Overpeck for the
eastern USA, using pollen data.
7121,000 cal 18,000 14C yr B.P. J.W. Williams.
2004. Variations in tree cover in North America
since the last glacial maximum, Global and
Planetary Change
7212,000 cal yr 10,500 14C yr B.P. Shuman et
al. (2002)
7311,000 14C yr B.P.
740
Analyst Eric C. Grimm
75Late Arrivals Fagus Tsuga at 7000 14C yr BP
MODIS 9/17/2003
76Fagus grandifolia (Beech)
77Tsuga canadensis (Eastern Hemlock)
788000 14C yr B.P. maximum aridity on the Great
Plains Southern boreal forest ecotone shifted
80 km northwards
796 ka climate Expression of maximum warmth in the
Midwest
Prairie peninsula (Transeau, 1935)
80Climate Model ComparisonsThese maps represent
the differences between Growing Degree Days (GDD)
for 6,000 years ago and today. The upper nine
maps were produced by climate simulations from
different models, while the map on the lower
right represents the same GDD difference inferred
from pollen.
http//www.geo.brown.edu/georesearch/esh/QE/QEHome
.html
81Reconstruction by R. Webb J. Overpeck for the
eastern USA.
82Medieval Warm Period AD 800-1200
83Cahokia
84Little Ice Age
Forest Composition 1800 as Interpreted from GLO
Survey Notes by MNIF
85Figure 13-8Page 286
Projected increase 1.5 6ºC Most think 2 4ºC
86Present range
Future range
Overlap
87- Pollen Personalities
- 1. Tom Webb, Dept. of Geological Sciences, Brown
Univ.
Paige Newby
88- A)Pollen Personalities
- 2. Margaret Davis, Dept. of Ecology, Univ. of
Minnesota
Ph.D., Harvard University, 1957
89- A) Pollen Personalities
- 3. Jonathan Overpeck
- Was at NOAA/NGDC Paleoclimatology Program, and
INSTAAR, University of Colorado, Boulder - Now Professor of Geosciences, U of Arizona
90- A) Pollen Personalities
- Jim Ritchie
- Father of Canadian pollen analysis
- Was at U of Toronto (advisor of Glen MacDonald,
UCLA) - Retired to Ireland
91- A) Pollen Personalities
- 5. Glen MacDonald
- Dept of Geography, UCLA
- Was at McMaster Univ. in Ontario
92- A) Pollen Personalities
- 6. The Delcourts
- Hazel R. Delcourt Paul A. Delcourt
- Dept. of Ecology Evol Biology,U of Tennessee
93- A) Pollen Personalities
- 7. Patrick Bartlein, Dept. of Geography, U of
Oregon (Eugene) - climatologist data modeler
94- A) Pollen Personalities
- 8. Jock McAndrews, Dept. of Botany, U of Toronto
- Great Lakes climate reconstruction aboriginal
impacts
95- A) Pollen Personalities
- 8. Jock McAndrews, Dept. of Botany, U of Toronto
- Great Lakes climate reconstruction aboriginal
impacts
Crawford Lake, Ontario Iroquoian villages corn
fields
96- A) Pollen Personalities
- 9. Herb Wright Jr., Prof. Emeritis, Dept. of
Geology Geophysics, U of Minnesota - Ph.D . 1943 Harvard
- University, Geology
- Synthesis papers
- 1960s-1990s
- Founder of the LRC
- Livingston corer
- Geologic history
97- A) Pollen Personalities
- 10. Ronald Kapp, Alma College, MI
- Ronald O. Kapp Memorial Prairie on the west side
of the Coolbough Natural Areas
98- A) Pollen Personalities
- 11. Eric Grimm, Illinois State Museum
- Research in Great Plains, Illinois, Florida
- Creator of Tilia Tilia.graph pollen data
plotting software
Eric
99- A) Pollen Personalities
- 12. Lou Maher, Dept. of Geological Sci., Univ. of
Wisconsin-Madison