introduction to tree rings & dendrochronology · radiocarbon dating) p 52 . now on to the g-3...
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TOPIC #9
INTRODUCTION
TO TREE RINGS &
DENDROCHRONOLOGY
CLASS NOTES p 51
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Global Change Tools
TREE RINGS &
NATURAL ARCHIVES
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DETECTING GLOBAL WARMING:
In the recent past, we use the “INSTRUMENTAL
RECORD” based on actual Thermometer
readings from around the globe
From Dire Predictions, p 36
Temperature
Trends
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We looked at some of these during this
Indicator Interlude . . . Remember these
time series “anomaly” plots?
p 45
These temperature records and graphs are available online at the National
Climatic Data Center (NCDC) of NOAA (The National Oceanic & Atmospheric
Administration): http://www.ncdc.noaa.gov/cmb-faq/anomalies.php
But what about what happened long
before the Industrial Revolution?
Don’t we really need to look at temperatures
from a LONG time ago to assess the severity
of the recent temperature observations of
warming?
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1) a long-term temperature record, i.e., centuries
2) over a large part of the globe
3) To be able to say . . . . .
“What's the average been for several hundred
years, & is this a significant departure from that?”
“And that's very difficult to do.”
(James Trefil, physicist)
To make an incontrovertible case about
the role that humans play in global
warming, what do scientists need?
Review: p 17
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Trees and stones will teach you that which you can never learn from masters.
~ St. Bernard of Clairvaux
p 51
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“PROXY” DATA or
NATURAL ARCHIVES of CLIMATE
Corals
Ice cores
Pollen
Tree rings! Lake, bog &
ocean
sediments
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TOPIC #9
INTRODUCTION
TO TREE RINGS &
DENDROCHRONOLOGY
CLASS NOTES p 51
![Page 9: INTRODUCTION TO TREE RINGS & DENDROCHRONOLOGY · radiocarbon dating) p 52 . Now on to the G-3 Tree-Ring “Wood Kit” ASSIGNMENT! Goals of Assignment G-3: (1) To see “inside”](https://reader034.vdocuments.us/reader034/viewer/2022043001/5f7b9e9dd1534778945e21ef/html5/thumbnails/9.jpg)
Dendrochronology is the dating
and study of annual rings in trees:
•dendros: from trees, or more specifically the growth rings of trees
•chronos: time, or more specifically events in past time
•ology: the study of . . .
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Partial
cross-section
of a coniferous
tree
How old is it?
(in complete
years) count ‘em!
7 years old
(now in 8th year
of growth) P 51
The current year’s
actively growing
cells are just
underneath the bark
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P 51
With 7 rings in
the cross-
section,
Is this the
tree’s age?
It depends on
the height of
the sample
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With 7 rings in
the cross-
section,
Is this the
tree’s age?
It depends on
the height of
the sample More
rings
Fewer
rings
Trees grow from the top
http://www.jefpat.org/Wood&CharcoalIdentification/Wood&Charcoal_Part2.htm
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Clicker Question:
Given what you just learned about how trees grow,
what is wrong with this picture?
A. Trees grow up, not out,
so this is clearly a photo
shopped image.
B. In 99 years of tree
growth, the bicycle would
be much higher up in the
tree.
C. In 99 years of tree
growth, the bicycle would
still be on the ground, but
the tree would have started
to grow around it.
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Conifer Tree Ring (cross-section view)
Why we can see the rings: cell size & thickness
changes during the growing season
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•Earlywood:
•Cells: thin walls, large diameter •Appears light in color
•Latewood: •Cells: thick walls, small diameter •Appears dark in color
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Ring Porous Angiosperm Tree Ring (cross-section, view)
•Earlywood:
•Cells: large diameter vessels •Latewood:
•Cells: small diameter vessels
But
not all
trees
have
rings!
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The image below shows a conifer tree-ring sample with about thirty rings (every tenth ring is marked) – growing from left to right. The rings display much variation:
Pith Bark (center of tree) (outside of tree)
Tree growth (adding new cells) is this way
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Variation in tree rings is due to
variation in environmental
conditions when they were
formed.
• dry or moist soil conditions
• cold or warm temperatures
• frost rings from tissue damage
• even insect outbreaks, fires, and
other non-climatic factors
Studying this variation gives us
information about past environmental
conditions and is the basis for many
research applications of
dendrochronology.
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How do we get the
tree rings without
killing the trees!
Extract
cores with
an
increment
borer
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If the tree is
already dead or
cut down, we
can take cross-
sections from
the tree or its
stump
Notice how wide
the rings in the
center are
– this was when
the tree was
young and
growing faster!
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KEY PRINCIPLES OF
DENDROCHRONOLOGY
UNIFORMITARIANISM –
“The present is the key to the past”
(this is a key principle for many other natural
archives used in the geological sciences as well)
Key
Principles
p 51
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LIMITING FACTORS –
growth can occur only as fast as allowed
by the factor that is most limiting, e.g.
• “too dry” – the amount rainfall is the limiting
factor
• “too cold” or “too hot” – the temperature is
the limiting factor
• NOTE: the limiting factor can vary from site
to site, even in the same species of tree!
Key
Principles
p 51
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SITE
SELECTION --
sites are selected
based on criteria
of tree-ring
sensitivity to an
environmental
variable
(temperature,
precipitation, etc.) Key
Principles
p 51
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Complacent Sensitive p 52
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B
B 1900 1910
A
A
1920 1930
C
C 1890 1880 1870 1860 1850
Crossdating: The Central Premise of
Dendrochronology
<<< “Bridging” the record back in time <<< Key
Principles
p 51
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CROSSDATING –
matching patterns in rings of several
sensitive tree-ring series allows
precise dating to exact year
Key
Principles
p 51
To Crossdate
you need a lot of
rings to
compare, usually
50 rings
minimum to be
certain of dating
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Now, back to the principles:
REPLICATION –
“noise” minimized by sampling many trees at
a site + more than one core per tree
Key
Principles
p 51
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Ring width measurements showing a
similar pattern of growth
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ECOLOGICAL
AMPLITUDE –
trees are more
sensitive to their
environment at
latitudinal and
elevational limits
of the tree
species’ range
Very old tree on Mt Graham,
SE Arizona
inner ring date: A.D. 1101
Key
Principles
p 51
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KEY SCIENTIFIC ISSUES
• Missing rings & false rings (to identify
these, need a “master chronology”)
• Species limitations (some trees have no
rings, non-annual rings, or poorly defined
rings)
• Trees must crossdate! (can’t develop a
chronology or link to climate without this)
Top of
p 52
Today’s class activity
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• Geographical limitations
tropics, deserts and other
treeless areas, oceans, etc.)
p 52
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• Age
limitations
old trees hard
to find
oldest living
trees =
Bristlecone
Pines
~ 5,000 years old
why don’t we
know for certain? p 52
Because sampling the base
of a live tree is difficult
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• Value of precise dating
(long chronologies, climate
reconstructions, archaeology,
radiocarbon dating)
p 52
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Now on to the G-3
Tree-Ring “Wood Kit”
ASSIGNMENT!
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Goals of Assignment G-3:
(1) To see “inside” different species of
trees and woody shrubs
(2) To classify the wood samples in a
“wood kit” into categories :
Trees that are:
(1) Suitable or
(2) Unsuitable
. . . for crossdating and subsequent
dendrochronological analysis.
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SUMMARY OF FEATURES THAT INDICATE
SUITABILITY FOR DENDROCHRONOLOGY
See bottom of p 53 and pp 121 -122 in Class Notes
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Then, for each specimen
in your box, fill out reasons
FOR using it and reasons for NOT
using it in a dendrochronological study
Start by matching
each wood specimen
with a PHOTO,
using LABELS on the
wood to guide you
Example:
SEGI = Giant redwood Southwestern white pine
(Pinus strobiformis))
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1) Match the wood specimens in your
box with the right tree photo
2) Fill our the chart for the specimens
in your box
3) SWAP boxes
4) REPEAT for second box
5) All who participated, sign the form
& return the folder with your
completed G-3 form inside
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SUMMARY OF FEATURES THAT INDICATE
SUITABILITY FOR DENDROCHRONOLOGY
See pp 121 -122 in Class Notes
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TIME TO WRAP UP FOR
TODAY
Please clean up your area
and put chairs back in
place