tree advancement patterns

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TREELINE ADVANCE P ATTERNS OF ALASKAN WHITE SPRUCE TREELINE ADVANCE P ATTERNS OF ALASKAN WHITE SPRUCE Keena Auld, Kenneth Chadwell, Turner Glasgow, David Cairns, and Keith Gaddis Texas A&M University Department of Geography, College Station, Texas Is P. glauca treeline advancing? Question Hypothesis 1. If treeline is advancing, trees establishment date will decrease (become more recent) as elevation increases 2. If treeline advance is not occurring, then there will be no relationship between elevation and tree establishment date Methods Lab Methods In the fall of 2015, we measured the establishment date of each tree by counting the tree rings on extracted tree cores. Abstract Many recent studies have indicated altitudinal treeline advance throughout the world due to global climatic changes. These advances have major implications for the assembly and survival of species throughout the world that may become marginalized as their habitat is destroyed by this advance. Given this fact, we set out to examine treeline advance patterns in the dominant North American treeline forming species, white spruce (Picea glauca) throughout south-central Alaska. We examined Dendrochronological data rom 17 sites and have found a variable arrangement of treeline pattern across the study area with some sites showing a clear pattern of advance and others maintaining stabile over the recent past. Background Treeline is an ecotone where the forest biome transitions to a tundra at the highest elevation point where trees can grow Changes in climate have a direct link the global treeline position. Long winters limit establishment of seeds and permafrost prevents deep roots from penetrating the soil. As global climates have warmed, forest biomes have began to encroach on that of the tundra leading to treeline advance. Study System White spruce (Picea glauca) is native to the boreal forest of North America. It has evergreen needles accompanied by narrow, oblong cones. The species disperses through seeds or layering (where lower branches take root to form new trunks that later separate from the maternal tree forming a clone). The area used in this study was south- central Alaska. The climate of region is subarctic with temperatures averaging -12 to 18 ˚C throughout the year. Climatic data has indicated a warming trend in this area. This region is heavily forested, with high mountainous terrain. Results Conclusion Treelines are advancing 5/17 show definite treeline advance 3-6 sites show younger trees at treeline Recent advance over a short spatial scale Topography determines advance The correlation between tree age and distance from treeline was explained by the slope at the sample site. Low sloped sites have greater treeline advance rates. Acknowledgements Future Work How does climate influence advance? We will determine if contemporary climate to influence advance rates. We will use climate modelling to identify if areas with greatest climatic change have experienced greater advance. We will analyze additional topographic variables (slope, aspect, curvature) How do dispersal and reproduction affect influence treeline advance? We will relate this work to our existing analysis of dispersal and reproductive pattern using genetics. Treeline Advance Infilling No Pattern We would like to thank Rachel Clausing, Zac Harlow, and Michelle Lee for tireless field collection. Clint Magill provided guidance and laboratory resources to conduct genetic work. Parveen Chhetri assisted in lab work and analysis. 1840 1860 1880 1900 1920 1940 1960 1980 2000 2020 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 16 P-value > 0.05 1900 1920 1940 1960 1980 2000 2020 2040 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 20 P-value > 0.05 1750 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 25 P-value > 0.05 1900 1920 1940 1960 1980 2000 2020 2040 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 28 P-value > 0.05 1750 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 32 P-value > 0.05 1750 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 33 Adjusted R-squred: 0.08 P-value < 0.05 1450 1550 1650 1750 1850 1950 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 34 P-value > 0.05 1860 1880 1900 1920 1940 1960 1980 2000 2020 2040 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 41 Adjusted R-squred: 0.27 P-value < 0.001 1650 1700 1750 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 36 Adjusted R-squred: 0.10 P-value < 0.05 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 EStablishment Year Distance From Treeline (m) Site 43 P-value > 0.05 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 46 P-value > 0.05 1650 1700 1750 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 55 P-value > 0.05 1900 1920 1940 1960 1980 2000 2020 2040 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 58 Adjusted R-squred: 0.25 P-value < 0.001 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishmnet Year Distance From Treeline (m) Site 68 Adjusted R-squred: 0.28 P-value < 0.001 1860 1880 1900 1920 1940 1960 1980 2000 2020 2040 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 71 P-value > 0.05 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 75 Adjusted R-squred: 0.19 P-value < 0.001 1650 1700 1750 1800 1850 1900 1950 2000 2050 0 100 200 300 400 500 600 Establishment Year Distance From Treeline (m) Site 76 P-value > 0.05 Field Methods In the summer of 2015, we sampled cores from trees spaced on 500 m transects parallel and perpendicular to treeline. Five trees were sampled every 50 m. We collected a total of 1,870 white spruce tree cores across 17 sites. Analysis We used linear regression to examine the age of trees relative to the distance from treeline. An additional analysis examining topographic effects was conducted using logistic regression y = 0.0569ln(x) + 0.0805 R² = 0.3586 -0.25 -0.2 -0.15 -0.1 -0.05 0 0.05 0.1 0.15 0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 Correlation Coefficient (r) Slope of Sample Site Does topography influence treeline advance ? We conducted a preliminary analysis to examine topographic effects (slope at each sample site) on treeline advance, using a logistic regression.

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Page 1: Tree Advancement Patterns

TREELINE ADVANCE PATTERNS OF ALASKAN WHITE SPRUCE TREELINE ADVANCE PATTERNS OF ALASKAN WHITE SPRUCE Keena Auld, Kenneth Chadwell, Turner Glasgow, David Cairns, and Keith Gaddis

Texas A&M University Department of Geography, College Station, Texas

Is P. glauca treeline advancing?

Question

Hypothesis

1. If treeline is advancing, trees

establishment date will decrease (become

more recent) as elevation increases

2. If treeline advance is not occurring, then

there will be no relationship between

elevation and tree establishment date

Methods

Lab Methods

In the fall of 2015, we

measured the

establishment date of

each tree by counting

the tree rings on

extracted tree cores.

Abstract Many recent studies have indicated altitudinal

treeline advance throughout the world due to global

climatic changes. These advances have major

implications for the assembly and survival of

species throughout the world that may become

marginalized as their habitat is destroyed by this

advance. Given this fact, we set out to examine

treeline advance patterns in the dominant North

American treeline forming species, white spruce

(Picea glauca) throughout south-central Alaska.

We examined Dendrochronological data rom 17

sites and have found a variable arrangement of

treeline pattern across the study area with some

sites showing a clear pattern of advance and others

maintaining stabile over the recent past.

Background

Treeline is an ecotone

where the forest biome

transitions to a tundra at

the highest elevation point

where trees can grow

Changes in climate have a

direct link the global treeline

position. Long winters limit

establishment of seeds and

permafrost prevents deep roots

from penetrating the soil. As

global climates have warmed,

forest biomes have began to

encroach on that of the tundra

leading to treeline advance.

Study System White spruce (Picea glauca) is

native to the boreal forest of

North America. It has

evergreen needles

accompanied by narrow,

oblong cones. The species

disperses through seeds or

layering (where lower branches

take root to form new trunks

that later separate from the

maternal tree forming a clone).

The area used in this study was south-

central Alaska. The climate of region is

subarctic with temperatures averaging -12

to 18 ˚C throughout the year. Climatic data

has indicated a warming trend in this area.

This region is heavily forested, with high

mountainous terrain.

Results Conclusion

Treelines are advancing

• 5/17 show definite treeline advance

• 3-6 sites show younger trees at treeline

• Recent advance over a short spatial scale

Topography determines advance

• The correlation between tree age and

distance from treeline was explained by

the slope at the sample site.

• Low sloped sites have greater treeline

advance rates.

Acknowledgements

Future Work

How does climate influence advance?

• We will determine if contemporary climate

to influence advance rates.

• We will use climate modelling to identify if

areas with greatest climatic change have

experienced greater advance.

• We will analyze additional topographic

variables (slope, aspect, curvature)

How do dispersal and reproduction

affect influence treeline advance?

• We will relate this work to our existing

analysis of dispersal and reproductive

pattern using genetics.

Treeline Advance

Infilling

No Pattern

We would like to thank Rachel Clausing, Zac

Harlow, and Michelle Lee for tireless field collection.

Clint Magill provided guidance and laboratory

resources to conduct genetic work. Parveen Chhetri

assisted in lab work and analysis.

No double space

P-vales to log

1840186018801900192019401960198020002020

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 16 P-value > 0.05

1900

1920

1940

1960

1980

2000

2020

2040

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 20 P-value > 0.05

1750

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 25 P-value > 0.05

1900

1920

1940

1960

1980

2000

2020

2040

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 28 P-value > 0.05

1750

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 32 P-value > 0.05

1750

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 33 Adjusted R-squred: 0.08 P-value < 0.05

1450

1550

1650

1750

1850

1950

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 34 P-value > 0.05

1860188019001920194019601980200020202040

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 41 Adjusted R-squred: 0.27 P-value < 0.001

1650

1700

1750

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 36 Adjusted R-squred: 0.10 P-value < 0.05

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

ESta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 43 P-value > 0.05

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 46 P-value > 0.05

1650

1700

1750

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 55 P-value > 0.05

1900

1920

1940

1960

1980

2000

2020

2040

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 58 Adjusted R-squred: 0.25 P-value < 0.001

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

net

Ye

ar

Distance From Treeline (m)

Site 68 Adjusted R-squred: 0.28 P-value < 0.001

1860188019001920194019601980200020202040

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 71 P-value > 0.05

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 75 Adjusted R-squred: 0.19 P-value < 0.001

1650

1700

1750

1800

1850

1900

1950

2000

2050

0 100 200 300 400 500 600

Esta

blis

hm

en

t Y

ear

Distance From Treeline (m)

Site 76 P-value > 0.05

Field Methods

In the summer of 2015,

we sampled cores from

trees spaced on 500 m

transects parallel and

perpendicular to

treeline. Five trees were

sampled every 50 m.

We collected a total of

1,870 white spruce tree

cores across 17 sites.

Analysis

We used linear regression to

examine the age of trees

relative to the distance from

treeline. An additional analysis

examining topographic effects

was conducted using logistic

regression

y = 0.0569ln(x) + 0.0805 R² = 0.3586

-0.25

-0.2

-0.15

-0.1

-0.05

0

0.05

0.1

0.15

0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4

Co

rre

lati

on

Co

effi

cie

nt

(r)

Slope of Sample Site

Does topography influence treeline advance ?

We conducted a

preliminary analysis

to examine

topographic effects

(slope at each

sample site) on

treeline advance,

using a logistic

regression.