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How do we know tree rings are annual?
The “pinning” method   Photograph: Keith Weston
Band dendrometer
Photograph: Baillie (1982)
P R I N C I P L E S O F C R O S S - DAT I N G
Scots pine
                                  Pinus sylvestris
Photograph: Fritz Schweingruber
temperature   water   day length
Climate acts to synchronize growth rates at the
level of the cell, the tree, the forest and beyond.
“ RINGS
    IN THE BRANCHES OF
    SAWED TREES SHOW
THE NUMBER OF YEARS
  AND, ACCORDING TO THEIR
     THICKNESS,
   THE YEARS WHICH WERE
        MORE OR LESS
          DRY. ”
      Leonardo da Vinci
Tree-ring width is not just a
  function of wet and dry
THE PRINCIPLE OF LIMITING FACTORS

 The rates of biological processes in trees, including the
 formation of woody cells, are constrained by the primary
 environmental variable that is most limiting.
temperature   water   day length
Same environmental forcings




                                      Similar
                              growth pa erns
THE PRINCIPLE OF CROSS-DATING

Matching pa erns in tree-ring widths or other ring characteristics
(such as ring density) among several trees allow the identification
of the exact year in which each ring was formed.
How cross-dating works.
Photograph: Dan Griffin
When was the outer ring formed?
Why can’t you just count the rings back in time?
COMPLICATION #1

  “Micro” rings
Ponderosa pine
                          Pinus ponderosa

Photograph: Peter Brown
COMPLICATION #2

   Partial rings
Limber pine
Pinus flexilis
COMPLICATION #3

  Missing rings
Picture not available.
A “missing ring” is a term used to describe the phenomenon
where a tree does not form wood around its trunk during a
                    single growing season.
A “missing ring” is a term used to describe the phenomenon
where a tree does not form wood around its trunk during a
                    single growing season.

 At the position where the tree-ring sample was collected!
COMPLICATION #4

   False rings
Ponderosa pine
                          Pinus ponderosa

Photograph: Peter Brown
Arizona cypress
                          Cupressus arizonica

Photograph: Peter Brown
False
ring boundary
                  sharp




 gradual
                    Annual
                ring boundary
COMPLICATION #5

  No outer date
Photo: Erik Nielsen
47
Photo: Erik Nielsen
48
THE PRINCIPLE OF CROSS-DATING

                          1900            1910              1920              1930




                              Two Douglas-fir cores from Eldorado Canyon, CO


Graphic: Jeff Lukas, INSTAAR
THE ‘LIST’ METHOD
S K E L E TO N P LOT T I N G
Photograph: Baillie (1982)
Ring width




             Tree age
Compare rings to their neighbors.
Marking tree-ring specimens for dating

                 decade

                 half-century

                 century

                 millennium
RING MEASUREMENT
Source: Hughes and Brown, 1992
Widespread drought caused narrow rings
  to form across the southwest USA
  during 1748 and 1750.




Source: Kurt Kipfmueller
What kind of trees have rings that can be
dated?

    • They have distinct and detectable rings.
    • Their rings must be reliably annual.
    • The formation of their rings must be
     sensitive to environmental conditions.

    • That sensitivity must cause the rings to
     vary from year to year.

    • Several trees must share common
     pa erns in tree-ring width, wood
     density or some other wood variable.
‘Complacent’
‘Complacent’ tree-ring series:
    • exhibit very li le year-to-year variation.
    • grow in se ings where the limiting growth
      factor doesn’t change much.
    • are tough to cross-date.
‘Sensitive’
‘Complacent’ tree-ring series:
    • exhibit very li le year-to-year variation.
    • grow in se ings where the limiting growth
      factor doesn’t change much.
    • are tough to cross-date.

‘Sensitive’ tree-ring series:
     • have wide and narrow rings that are
       intermixed through time.
     • Found in environments where the limiting
       factor is highly variable year to year
     • Matching ring pa erns across trees is
       easier.
Tucson AZ
PRE-WORK ASSIGNMENT

Before next class, try cross-dating online
h p://www.ltrr.arizona.edu/skeletonplot/introcrossdate.htm

              or google ‘LTRR skeleton plot’
P R I N C I P L E S O F C R O S S - DAT I N G

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