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Eastern Hemlock

Latin name:
Tsuga canadensis

Extracted from a waterfront pier near Wilmington, Delaware, the tree used to make this portion of the pier
actually came from a forest located in central Pennsylvania. The outermost tree ring dates to the late 1830s.

Giant Sequoia

Latin name:
Sequoiadendron giganteum

A close up of numerous fire scars on a giant sequoia cross section from Sequoia National Park in California, dating back well prior to A.D. 1000. Look closely! Can you find the sad bearded face cradled by his hands, as if he was crying?


Latin name:
Pseudotsuga menziesii

This photo shows the tree rings from a beam extracted many years ago from a pueblo in northeastern Arizona. The section shows many false rings and many micro-rings, suggesting this tree may have been growing in a marginal environment.

Ponderosa Pine

Latin name:
Pinus ponderosa

Close up of tree rings of a ponderosa pine collected at El Malpais National Monument in New Mexico, USA, showing tree rings centered around A.D. 1400. Notice the variability in ring widths indicative of sensitivity to year-to-year variation in precipitation.


Latin name:
Pseudotsuga menziesii

Perhaps my most requested image of tree rings, obtained from a small Douglas-fir growing in the Zuni Mountains of west-central New Mexico by my colleagues Rex Adams and Chris Baisan. Not very old, but has some of the most beautiful rings of all my displays!

White Oak

Latin name:
Quercus alba

Oak cores from the Hoskins House in Greensboro, North Carolina, site of a famous battle during the Revolutionary War. The house was built from trees cut in 1811 to 1813, not cut and built in the 1780s as the historical agency had hoped.

Ponderosa Pine

Latin name:
Pinus ponderosa

This ponderosa pine once grew at El Morro National Monument in New Mexico, USA, and was cut many years ago. Once you get up close to the stump, you can see a very old scar from a fire many hundreds of years ago that scarred the tree when it only about 12 years old!

Bahamian Pine

Latin name:
Pinus caribaea var. bahamensis

We collected many cross sections of Bahamian pines that had been cut for an industrial park on the island of Abaco, but the rings are very difficult to date! Many false rings, and the pine appears to terminate tree growth during the dry season.

Longleaf Pine

Latin name:
Pinus palustris

This cross section was one of many that came from an old crib dam across a creek that was exposed after a modern dam broke in Hope Mills, North Carolina in 2003. Such sections from old-growth longleaf pines are very rare and provide information on climate back to AD 1500!

White Oak

Latin name:
Quercus alba

Sometimes you don't have to look far to find beauty in wood, and sometimes it may not be a living tree! After an oak tree was cut a year or two before this section was obtained, decay fungi had already set in, beginning to break the wood down to its basic elements.

Southwestern White Pine

Latin name:
Pinus strobiformis

I collected this fire-scarred pine on Mt. Graham in southern Arizona in fall 1991, and it remains one of the best examples of how we can determine the season of fire by looking at the position of the scar within the ring.

Bristlecone Pine

Latin name:
Pinus longaeva

Bristlecone pines have become one of the best proxy records for those who study the history of volcanic eruptions because the cool temperatures caused by these eruptions create "frost rings" that form when the cells implode from the cold.

Eastern Redcedar

Latin name:
Juniperus virginiana

Many well-preserved eastern redcedar sections have been recovered from prehistoric sites in eastern Tennessee, and they have more than enough rings to date, but we don't have a long enough living-tree reference chronology to overlap with them!

Red Oak

Latin name:
Quercus rubra

Oak is by far the most common genus we find in the many historic structures we date using tree rings in the Southeastern U.S. The genus has good ring variability and rarely has problem rings. This section came from a historic tavern in Lexington, Virginia.

Sugar Maple

Latin name:
Acer saccharum

Maple, birch, beech, and basswood are all examples of hardwood species that form diffuse porous wood, meaning that the ring contains many small-diameter vessels all through the ring. Identifying the ring boundary on this wood type is a challenge to tree-ring scientists.

Live Oak

Latin name:
Quercus virginiana

Live oak is an example of an evergreen oak, which is not common within this genus. As such, the wood is semi-ring porous and the rings are very difficult to see and date. Ring growth is also very erratic, not forming the concentric around the tree that we require.


Latin name:
Pseudotsuga menziesii

These cores were collected on Mt. Graham in southern Arizona and show a major suppression event beginning in 1685 when missing rings became evident, followed by many micro-rings. This suppression was caused by a major wildfire in 1685!

Ponderosa Pine

Latin name:
Pinus ponderosa

I find it amazing what trees can record in their tree rings! Here we see a cross section of a pine that was damaged by a major flood in the year 1945 in the Chiricahua Mountains of southern Arizona. Notice the reaction wood that formed afterward.

Pignut Hickory

Latin name:
Carya glabra

Sometimes gray-scale imagery helps define tree rings when measuring. Although classified as "ring porous" species, the rather ill-defined tree rings in hickory tree species form large earlywood vessels and smaller latewoood vessels.

Subalpine Fir

Latin name:
Abies lasiocarpa

Decay has set in on the tree rings of this dead and downed subalpine fir that once grew on Apex Mountain in British Columbia, Canada, but the tree rings can still be measured and crossdated despite this!

White Fir

Latin name:
Abies concolor

We found a beautiful fire scar on this white fir that was used to build a cabin in the Valles Caldera of New Mexico. Thought to have been built in the early 1900s, we instead found the cabin was built form white fir and Douglas-fir trees cut in 1941.

Overcup Oak

Latin name:
Quercus lyrata

These oak cores were collected in northeastern Arkansas to investigate a change in the hydrologic regime of a wildlife refuge beginning in the 1990s. We found that trees at this site experienced a major disturbance event in the 1960s.

Western Juniper

Latin name:
Juniperus occidentalis

Near Frederick Butte in central Oregon, we discovered an unusual stand of western junipers that had the most unusual lobate growth forms we had ever seen. This site yielded a drought-sensitive chronology dating back to the AD 800s!

West Indies Pine

Latin name:
Pinus occidentalis

Above 3000 meters on the highest peak in the Carribean, we found an entire forest of these pines, many with fire scars, living on a steep rocky slope. The forest looked more like the dry ponderosa pine forests of the western U.S.

Whitebark Pine

Latin name:
Pinus albicaulis

Whitebark pines growing in the northern Rockies of the western U.S. can grow to be over 1,000 years old, but the species is slowly being decimated by the introduced white pine blister rust. Many of these ancient trees are now dead with ghostly white trunks.

Shagbark Hickory

Latin name:
Carya ovata

Curiously, tree-ring scientists rarely analyze some of the more common hardwood species in the eastern U.S., such as this hickory, perhaps because such forest interior trees may contain a weak climate signal necessary for crossdating.

Virginia Pine

Latin name:
Pinus virginiana

Blue stain found in many sections of dead pines (both in the western and eastern U.S.) is caused by a fungus carried by a pine beetle. The fungus spreads into the phloem and sapwood of living and dead pines, sometimes creating stunning patterns!

Pinyon Pine

Latin name:
Pinus edulis

Burned sections of pinyon pine are commonly found in archaeological sites in the southwestern U.S. These sections can be carefully broken or surfaced with a razor to reveal the ring structure inside to assist in dating the years of construction of the site.

Red Spruce

Latin name:
Picea rubens

Conifers in the highest elevations of the Appalachians of the eastern U.S., such as this red spruce, don't experience wildfires very often, but when fires do occur, they can create numerous fire scars even in this fire-intolerant species. Notice the growth release!

White Spruce

Latin name:
Picea glauca

This tree was located in the Canadian Rockies on the toe slope of an active avalanche path. The scar was created by a debris flow or snow avalanche which struck the tree, killing a section of the living tissue. The avalanche can therefore be dated to its exact year!

Engelmann Spruce

Latin name:
Picea engelmannii

I worked considerably in the spruce-fir forests of southern Arizona in my earliest years in dendrochronology, and learned that trees with limited sensitivity can provide a vast amount of information on the history of these forests.

Ponderosa Pine

Latin name:
Pinus ponderosa

The lava flows of El Malpais National Monument in New Mexico contain vast amounts of remnant wood, mostly ponderosa pines such as this sample, and the tree rings on these samples go back nearly 2000 years! Notice the year AD 1400 on this section.

Chestnut Oak

Latin name:
Quercus montana

In the southeastern U.S., hardwood species are often scarred by wildfire. Most often, this also will cause considerable decay in the sample, but this oak had several well preserved fire scars, suggesting fire was common in these drier, lower elevation sites.

Ponderosa Pine

Latin name:
Pinus ponderosa

I originally sampled this stump in 1991 for its fire scars, located in El Malpais National Monument of New Mexico. I found it again 20 years later and was happy you could still see the tree rings and fire scars clearly! It had originally been logged in the 1930s!

Lodgepole Pine

Latin name:
Pinus contorta

This pine is found at higher elevations in the Rocky Mountains of the western U.S. At this site in Montana, we had thought we found fire scars on these pines, but it turns out that these are scars caused by bark beetles stripping away portions of the bark.


Latin name:
Pseudotsuga menziesii

These cores illustrate the level of sensitivity to climate fluctuations in Douglas-fir trees growing in El Malpais National Monument in New Mexico. These rings show the common pattern of narrow marker rings between 1800 (on the left) and 1860 (on the right).


Latin name:
Pseudotsuga menziesii

This photo shows a close-up of the rings in the previous image. The very wide tree ring is the year 1816, the "Year Without a Summer." Cooler temperatures meant more soil water for the malpais Douglas-firs, causing a wide ring for that year!

Ponderosa Pine

Latin name:
Pinus ponderosa

Dating fire scars found in the annual rings is a major application of tree-ring dating. This photo shows two scars. Notice the wider rings that formed after the upper scar, perhaps caused by removal of competing vegetation or added nutrients.

Longleaf Pine

Latin name:
Pinus palustris

Longleaf pines have the greatest ages of all the eastern pines. They grow slowly in sandy soils of the Atlantic Coastal Plain, and have proven ideal for learning about past climate and disturbance events, if old-growth stands can be located!

Rocky Mountain Juniper

Latin name:
Juniperus scopulorum

The juniper species of the western U.S. have proven a challenge in tree-ring dating, but Rocky Mountain juniper has tree rings that are easily identified and can be crossdated. Just watch out for false rings and expanded latewood!


Latin name:
Pseudotsuga menziesii

A close-up photo of tree rings in Douglas-fir reveals the individual wood cells that make up the xylem. These are called "tracheids." Notice the change in cell wall thickness from the earlywood cells to the latewood cells along a radial file of cells.


Latin name:
Pseudotsuga menziesii

The best trees for learning about past climate will be those that grow to great ages and are particularly sensitive to year to year changes in climate. This Douglas-fir began growing around the year 200 BC and lived for nearly 1000 years!


Latin name:
Prosopis glandulosa

Some desert species from the mid-latitudes do form annual rings, but these diffuse-porous species have rings that are difficult to see. You can use black marker and white chalk dust to help bring out the rings! The dust fills the small vessels and the rings appear!

Norway Spruce

Latin name:
Picea abies

Spruce is the preferred genus for making high-quality wooden bodies on musical instruments. This photo shows the tree rings on the outer edge of the "Messiah" violin. Analysis of its tree rings helped show that the violin was contemporary with Stradivari!

Black Locust

Latin name:
Robinia pseudoacacia

In the eastern U.S., this common hardwood species has beautiful tree rings that demonstrate the ring porous wood type. The tree species, however, has some of the densest wood found in North America and is extremely difficult to core!

White Oak

Latin name:
Quercus alba

Oak is a major genus used to build log structures in the eastern U.S. Sometimes, however, we find that the individual trees experienced some major disturbances that caused very aberrant rings, making crossdating all but impossible.

Palo Verde

Latin name:
Parkinsonia florida

A common tree species in the American Southwest, palo verde is a diffuse porous species that forms very indistinct tree rings. As a result, little tree-ring research has been performed on this genus. Best to use complete cross sections, when available.

Ponderosa Pine

Latin name:
Pinus ponderosa

A major application of tree-ring research is learning about insect populations. For example, pandora moth defoliated the needles on this tree, causing some narrow rings to be produced. We can use this pattern to learn about insect populations over many centuries!

Table Mountain Pine

Latin name:
Pinus pungens

The analysis of fire scars in tree rings can also be applied to pine species growing in the eastern U.S. Table Mountain pine has proven to be the best species in the Appalachian Mountains for learning about past wildfires!

Subalpine Fir

Latin name:
Abies lasiocarpa

Subalpine fir grows in the highest elevations of the southern Rocky Mountains and forms fairly compacent ring series. Sometime between 1979 and 1980, this tree was stripped almost completely of its bark by a black bear, but it still survived in one small area!

Florida Torreya

Latin name:
Torreya taxifolia

Perhaps the rarest conifer in the U.S., this species is on the brink of extinction because its habitat is facing mounting pressure from rapid changes in its native environment. It forms very nice tree rings, but few adult individuals are left to analyze.

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Tips for Studying Tree Rings

Everyone who cores trees or analyzes tree rings at some point has found a way to do things faster and do them more efficiently. So, I collected all these tips over the years from the "masters" themselves, and added a few of mine! Have fun!


Increment Borer and Coring Tips
Field Equipment Tips
Laboratory Equipment Tips


Increment Borer and Coring Tips

Treat your borer with respect:

Increment borers are expensive, yet take a lot of abuse when we core trees. Keep these in top condition at all times. Be sure to clean the outside of the shaft with fine-grade steel wool and WD-40 to remove excess resin. When storing your borer, clean it inside and out with a gun-cleaning kit and WD-40, and coat the shaft and extractor with WD-40 before placing in storage.

Gun cleaning kit:

Cleaning the inside of your increment borer can be difficult, but not if you use: (1) a 22-caliber gun cleaning kit, and (2) lots of WD-40. Any department store will carry such kits in their sporting goods section. Be sure to get the kits used to clean 22-caliber rifles as these will have the extensions needed for your longer borers.

Latch hooks:

Have trouble keeping the latch hooked on your increment borer? Often when backing the borer out of a tree, the latch can come loose, causing the handle to come off. Go to the hardware store and buy some 0.5 inch rubber O-rings used in sink faucets. Slide these down the handle and over the latch when the borer is being used.

Sharpening kit:

Are your cores "ragged" when you pull them out of your borer? If so, your borer needs sharpening! A sharpening kit can be purchased from a forestry supplier, and comes with various shaped stones. Learn how to sharpen your borer, and keep your borer sharp, always! Otherwise, your cores will be ragged and will be prone to jamming up inside your borer!

Cleaning your borer:

Do cores tend to jam inside your borer? If so, then your borer needs (1) sharpening, (2) cleaning, or (3) both! Always make sure you head to the field with a sharp borer. At the end of each day, you should clean your borer with a gun cleaning kit and lots of lubricant. Debris and resin left inside your borer for long periods will cause chemical reactions that ultimately will pit and damage the inside of your borer, causing cores to jam regularly.

Fixing the extractor:

Does the extractor (or spoon) on your borer fail to grab the core when you insert it? First, make sure your extractor is as sharp as possible. Use the cone-shaped sharpening stone that came with your sharpening kit. Second, you may want to "clench" the end of the spoon near the teeth. Place a nail that's slightly narrower than the extractor inside the tip, and clench the extractor in a vise, using the nail as a guide. Don't clench too much, though.

V-handles for your borer:

Sometimes the straight handles on increment borers prevent coring in tight places (such as archaeological logs in cabins). Create a V-handle by scoring the handle on either side, bending into a V-shape, then welding the score line closed. A cross-brace can also help strengthen the borer.

Gloves for coring:

After coring many trees a day, your hands and fingers can become very sore. Purchase some fingerless gloves like those used by bicyclists and weight lifters, making sure they have padded palms, and your hands and fingers will be much less sore!

Flag your extractor:

Don't lose your extractor in the grass or leaf litter around the tree you're coring! If you accidentally step on it, you may not have a borer to use. Tie some bright colored flagging through the end loop on the extractor handle, and you'll never lose it again.

Extractor ethics:

Try not to place your extractor on the ground beside the tree as you can easily step on it and irreparably bend it. The ideal place? Wedge the extractor in some bark on the tree, if possible. If not, place it in your back pocket (my favorite), but be careful when you sit down!

Prevent jammed borers:

When coring, stop every few turns and insert the extractor until it reaches the core. Measure off the distance with your thumb on the end of the borer handle. Pull out the extractor and place it alongside the borer until the tip reaches the bark. If there is a discrepancy, your core is jamming!

Coring in tight places:

Sometimes the lower branches of trees (especially shrubby junipers) make coring difficult with those long handles. You do not have to use the handle that came with the borer -- the different lengths are interchangeable! So, you can core a tree with a 20 inch borer while turning the shaft with a 12 inch handle! Great when coring in tight places.

Stuck increment borer:

Sometimes our borers get stuck inside a tree. Be sure you have some parachute or heavy-duty cord with you. Tie a clove hitch around the shaft of the borer and wrap the other end of the cord around a nearby tree. Turn the handle counter-clockwise, thus tightening the rope. Be very careful, though, because the borer may come out of the tree with considerable force.

Extra borer leverage:

Sometimes coring a tree could be aided if you had additional leverage. Try this. Use a handle that comes from an increment borer one or two sizes larger than the one you're currently using. Be careful, though, because additional torque is applied to the auger by this longer handle.

Removing a jammed core:

If you do get a core stuck in your borer, check to see how much wood is compressed. If it's less than 2.5 cm (1 in), try this. Insert the extractor and turn the borer upside down, holding the extractor cap. Spin the borer with the other hand. After a while, you may remove enough wood to allow the extractor to slide beneath the jammed core.

Removing stuck cores:

If you jam your borer to the point it can't be unjammed in the field, take the auger back to a wood shop. Using a series of narrow to wider drill bits, use a table-mounted drill press to precision drill the jammed wood through the tip of the auger. Then clean out any residual wood with your gun cleaning kit.

"Pithing" a tree:

In some studies, pith (or near-pith) is required to accurately age the tree. (1) Be sure you pull the core as it was oriented in the tree. (2) Gauge by how far off you are (e.g., 1 cm) by looking at the curvature on innermost rings of your core. (3) Insert the extractor into the hole for a guide. (4) Take a second core, but offset the auger by the distance you are from pith. Keep it parallel to the extractor.


Field Equipment Tips

Cleaning your chains:

Are you sawing a lot of pines with your chain saw? If so, the chain can get gummed up with resin very quickly, thus reducing its cutting ability and performance. If you have any juniper logs nearby, run the chain through them. This will remove most of the resin on your chain, and rejuvenate your chain saw.

Plastic wrap:

Sometimes you may need to wrap your fragile cross sections so that they will stay together until you get them back to the lab. Purchase some plastic wrapping in 5 inch wide rolls (12.5 cm) (see my Supplies web page). Alternatively, you can use 2.5 inch (5.25 cm) strapping tape.

Fishing vest:

Don't have enough pockets for all your supplies while coring trees? Invest in a fishing vest! These have multiple pockets and can store items such as straws, dbh tape, flagging, and sharpening kit, as well as first aid supplies. Larger pockets in the vest can also be used to carry small-sized cross sections!

Wooden golf tees:

Ever get a small section of wood stuck in the tip of your borer? Never ever use the metal tip of your extractor! Instead, purchase some wooden golf tees from a sporting goods store. These will not damage the tip of your borer as you push out the stuck piece of wood.


Next time you visit an Oriental restaurant, save those chopsticks! Why? They are great for removing small pieces of wood stuck in the tip of your increment borer, and they won't damage your borer. Carry one or two in your field vest. Remember, never ever use the metal tip of your extractor!

Coring height gauge:

Dendrochronologists regularly record their coring height on a tree. A quick and instant height measure can be made by simply marking the handle of your increment borer with a black felt tip pen, such as a Sharpie, at every cm. After coring, hold this up to the trunk of the tree and record your coring height!

GPS units:

You should always record the location of your trees based on nearby markers and previously sampled trees. To help, invest in a hand-held GPS unit! The better ones (about $US 350-400) are remarkably accurate, and have even gotten me back to individual trees I previously sampled!

GPS your trees:

Modern hand-held Global Positioning Systems can quickly document precise locations of your sampled trees to the nearest 1-3 meters, handy in case you need to return to the field to collect cores from the oldest tree in your study, for example! I've found that dense tree cover mostly is not a concern for obtaining coordinates, either.

Waterproof notebooks:

Often, we have to sample while it's raining, and this can cause our field notes to become smudged and unreadable. Invest in some "Write-in-the Rain" brand field notebooks, available from Forestry Suppliers and other companies. They're low-cost and will save your field notes.

Pre-wrap those fragile cross-sections:

When collecting fragile samples for fire history analysis, I've found it very useful to wrap the sample tightly in-situ with plastic wrap prior to sawing with a chain saw. Make your top-cut first, wrap the sample, then make your bottom-cut. This will keep those fire scars from flying everywhere!

Check the top and bottom of the fire-scarred surface:

When collecting samples for fire history, don't assume the best sections will come from the middle of the scarred area. Often, the section containing the best scars will be located at the top and/or bottom of the scarred surface (also called a "catface"). If you can, collect sections from as many areas of the scarred area.

Chalk markers:

When conducting a complete inventory of all trees in a study plot for species composition and age structure analyses, mark trees that have been tallied using chalk markers available from most arts and crafts stores. These are the same types of markers used for writing "Just married" on the windshields of automobiles (thanks Elaine Kennedy Sutherland).

Mini dbh tapes:

When collecting tree information, dendrochronologists must carry a lot of supplies into the field. To save space, invest in the mini-sized diameter-at-breast-height ("dbh") tapes, capable of measuring trees up to two meters in diameter (but that's all). These are ultra-small and fit easily into a shirt pocket for easy access.

Portable hand drill and bit:

Sometimes we jam our borers in the field. To remove the jammed core, use a 6mm (0.25") drill bit that has been welded to a stock steel rod (any machine shop can do this). The final drill bit should be the length of your borer. You can use some duct tape wrapped around the end to hold the bit while you gently turn it inside the auger shaft (thanks Jeff Lukas).

Compressed air:

This is nifty. When using a dry wood borer at an archaeological or historic site, the sawdust can accumulate around the core. Buy cans of compressed air at an office supply store (used for cleaning computer parts) and every 12-15 mm (0.5 inch) or so, stop coring and blow out the sawdust!


Laboratory Equipment Tips

Core trays

Save those flat cardboard trays that canned cat food and dog food come packed on because these make great trays for sorting and storing your cores while you're working on them in the lab! Have one tray marked for cores being processed and another tray for cores that have been processed (for example, already crossdated and measured).

Pith locators:

Sometimes you need to estimate the age of a tree from cores that did not reach pith. Using graphics software, create templates of concentric circles (i.e., "ring") of various widths, e.g. every 1mm, 1.5mm, etc. Print these out on transparency film. To estimate the tree age, hold the template containing rings of the appropriate width over the innermost rings and age the tree.

Marking your rings:

I've seen that standard dissecting needles today are not very sharp. Try this. Rather than using a needle to pin-prick your rings once they're crossdated, use instead the lead on your mechanical pencil. This works only with softwoods, of course, and make sure you have thick lead (2H, 3B). In addition, you can sharpen your lead with fine-grade sandpaper (thanks Jeff Lukas).

Sharpen your dissecting needles:

We often use dissecting needles to put the final pin-pricks on decadal rings of crossdated pieces of wood. These tend to get dull and sometimes come shipped rather dull. Do this. Rub the tip of the needle back and forth across some fine-grade sandpaper, and then inspect the tip under a microscope until the desired sharpness is attained.

Clean your sanding belts:

Sanding belts are not cheap, so it's best to take care of them and make them last as long as possible. Few people realize you can clean the resin and debris off the belts using "belt cleaners." They come in various sizes, but the best are 25 cm long and 5 cm wide. For more information, check out my supplies page under "Sandpaper" at the bottom.

Gummy erasers:

Need to polish up a surface on a core (or section)? Cut a strip of fine sandpaper or sanding film (>= 320 grit) 2.5 cm wide by 10 cm long, and wrap this around an artist's gummy eraser (available at all art supply stores or from my online supplies page). The eraser will conform to the contours of the core!

Beanbags for your cores:

Sometimes when you're measuring, you have to position the core and its mount at an angle to help see the rings, especially if the core was mounted slightly twisted. To help re-position the core, make some small beanbags partially filled with lead shot wrapped in some sturdy cover, such as heavy plastic or leather. Place these around the core to hold it at the appropriate angle while measuring!

Graph paper:

It seems our favorite graph paper for creating skeleton plots is no longer made. On the "Supplies" page, click on "Laboratory supplies" and you'll see a link to a web site where you can download software for creating your very own green-tinted graph paper on your own color printer!

Scotch tape for core mounting:

This was a revelation when I learned this. I had been using masking tape for years, but Peter Brown taught me this trick! Once your core has been mounted in glue on your core mount, secure them tightly on the mount with a few strips of clear Scotch tape. And NO NEED to remove it before sanding! Just sand the core through the tape itself!

Dissecting needles:

Once the tree rings in your wood are correctly crossdated, you should "prick" holes permanently into your rings: one hole = every 10th decade ring, two holes = 50th mid-century ring, three holes = century ring, and four holes = millennium ring). To do this, use dissecting needles, also called biological probes. High-quality metal needles are worth the extra money.

Stabilizing wet wood:

Sometimes we wish to preserve entire sections of wet wood for analysis. Use a low-molecular liquid such as polyethylenglycol (PEG) 200 or PEG 400 to soak the wood in a PEG-bath. Low viscosity PEG 400 enables the liquid to spread in the wet wood. After drying, PEG acts as dimensional stabilizing agent in relation to moisture (thanks Rupert Wimmer).

Pegboard sanding surface:

To create a sanding table that will allow you to sand cross sections of any size, nail down pegboard (available from your home improvement store) unto a sturdy table with a wooden top. Also, purchase the correct size wooden pegs. Hammer these into the pegboard around your irregularly shaped cross section for a firm fit!

Map tubes:

Need a carrying case for your straws once you collect your cores? Go to a map store or mailing outlet (like Mailboxes Etc.) and buy those round mailing tubes in the length you require. I use one tube to store my unused straws and another to store my straws with the cores. Plastic works best, as paper tubes can become soggy if it rains.

Steel wool:

Need to get excess resin off your cores to see your rings? Burnish the surface lightly with fine-grade steel wool! This will remove the excess resin and enhance the ring boundaries.

Electric planers:

Need to get a flat surface on a cross section that has deep chain saw cuts? On large sections, use an electric hand planer to remove the saw cuts. On smaller sections, use a band saw to slice the section. Both techniques should result in a new, flatter surface on the section.

Black markers:

Are you working with cross sections from a tree species with rings difficult to see when sanded? Try this. Color half the section with black marker. Then spread baby powder over the colored half, rub in, and blow the remaining powder away. Rings (if any) should now be more prominent on the colored section. Compare this half with the original half.

Freezing sections:

Afraid of bringing home critters (ants, termites, and other critters) to your lab? This could be problematic if termites get into your wood collection. Take all pieces of wood to an herbarium or any place with a low temperature deep freezer. Place your sections in these overnight to ensure you don't have invasive insect problems.

Mold on your cores:

Does mold form inside your plastic straws on your valuable increment cores, thus masking your ring boundaries? As soon as possible, slit the plastic straws with a razor, thus allowing air in while allowing the moisture in the cores to wick away. This will prevent or reduce the amount of mold that forms on your increment cores.

Cardboard for mounting:

Running out of expensive plyboard to mount your fragile cross sections? Did you know that many cross sections can simply be mounted on sturdy corrugated cardboard, such as the cardboard found in boxes for shipping heavy items. I look for these on loading docks!

Fluorescent lighting for charcoal:

Tree rings on charcoal surfaces are difficult to see, often because of the reflection caused by regular incandescent lights found in standard microscope illuminators. Fluorescent lights (especially light rings) provide softer, cooler light that helps bring out tree-ring patterns on charcoal sections! And they are not that expensive.

"Crack" your charcoal:

The guys in the dendroarchaeology section of the tree-ring lab in Tucson taught me a neat trick to help bring out tree rings on charcoal pieces. Take the charcoal piece in both hands (if big enough) and carefully break the section in two along a transverse plane. If the piece is smaller, "flick" off a piece of charcoal from the surface with the edge of a razor blade. The rings should now stand out very nicely.

Document your cores:

When processing your valuable cores, the person responsible for each step in preparation should initial the bottom of the core mount. For example, "MS by GW" (mounted and sanded by GW), "XD by Joe H." (crossdated by Joe H.), and "ME by MS" (measured by MS). This technique ensures careful attention to these important steps by the technicians.




Be sure to check for "A" and "B" flags in your output. An "A" flag means COFECHA could not find an alternate dating position for a segment that correlates low with the other series. A "B" flag is more serious and means COFECHA found an alternate dating position. Systematic placements of flagged segments possibly indicates a misdated series.


Need help isolating a problem (missing or double) ring in a segment? Run COFECHA again a few times, decreasing the length of the segments being tested each time (e.g. 50 years, 40 years, then 30 years). Inspect the output and you'll notice you can zero in on the problem ring more efficiently. Then be sure to go to the wood and inspect that segment for the possible problem.


What constitutes a misdated segment or series in COFECHA? First, look for an r-value that's twice as high as that at the zero-shift position. Second, look for consecutive segments with the same suggested alternate placement, e.g. +1 or -1 (the two most common alternate placements). Third, look for an outlier ring listed by COFECHA at or around a known problem ring (most likely a missing or extremely narrow ring).


If you need to date some undated measurement series using already dated series, did you know you can save the master dating chronology created by COFECHA? In subsequent runs, enter the file name that contains the master chronology when COFECHA asks you for the "Crossdated tree-ring series." Then enter the file containing the undated series when prompted. The resulting output is much simpler to read and interpret!


See the graph with upper- and lower-case letters? This helps identify pointer years (extremely narrow or wide rings) as well as overall trends. The ampersand (@) symbol means a near average ring index, an upper-case letter means a year with overall wide rings, while a lower-case letter means a year with overall narrow rings. Each increment in the letter equals a 0.25 standard deviation unit!


If no reference chronology is handy, and you have many undated measurement series, first see if you have internal dating among them. These should all be measured beginning with year "0" or year "1." When asked to enter a dated series, hit return. Next, enter the name of the file containing the undated series, when prompted. COFECHA will then test each series against all others. Look for t-values at or above 3.5!


When attempting to date multiple undated series without a reference chronology or dated series, try not to overwhelm the analysis by analyzing too many series at once. Start with a few (8-12) of your measurement series with the clearest ring patterns, and enter these in COFECHA. As they become dated against each other, use one as the anchor and adjust all other relative dates accordingly.


Did you know you can use a reference index chronology as your dated series when attempting to date your undated measurement series? Simply enter the name of the file containing the index chronology when prompted for "Crossdated tree-ring series." COFECHA should recognize that this is an index chronology and not measurement series. If not, COFECHA will prompt you for the format. Simple!


Here's a tip that's sure to please. Sometimes you may want to use several index chronologies from a region to develop a single reference chronology to date some undated series. Place all index chronologies in one file (make sure they have the same format). Enter this file when prompted for "Crossdated tree-ring series." You may want to turn off detrending in COFECHA -- enter "-1" under the spline option.

COFECHA Tip #10:

Always archive your tree-ring measurements! In the Main Menu of COFECHA, you can choose the option that says "List Ring Measurements" and COFECHA will print out the measurements for each series in the output. Select this option when the measurements are completely and precisely dated, then place this output in a secure, permanent location!

COFECHA Tip #11:

If you're conducting many runs of COFECHA to diagnose the same data set, you don't have to print out the entire output produced by COFECHA. In the Main Menu, select option 8 and have COFECHA print out only those parts of the output you absolutely need, like the diagnostics in Part 6 or the results of dating an undated series in Part 8!

COFECHA Tip #12:

To help diagnose a possible location where a misdated segment may begin, carefully inspect Section C in Part 6 of the diagnostics. This section lists consecutive year-to-year changes that are very different from the mean change found in all other series. If consecutive years are listed (e.g. 1851 1852), this could be the location where a missing ring should be or a possible error in measurement.

COFECHA Tip #13:

So, what value of mean interseries correlation (first page in the box, and found in Part 7 at bottom) should you have? I consider a value of 0.40 the minimum a tree-ring data set should have. I've seen values much higher in the American Southwest (0.55 to 0.70) while data sets for eastern species may range from 0.45 to 0.60. Data sets with very long complacent series, however, may have values less than 0.40.

COFECHA Tip #14:

If you're developed a network of tree-ring chronologies in an area, you may want to check the final dating of the chronologies against each other, and to learn where the climate signal is the weakest. Did you know you can enter a series of chronologies from one file into COFECHA? Simply paste all the chronologies (Index or Compact format) one underneath another in one file!

COFECHA Tip #15:

Need help isolating a problem (missing or double) ring in a segment? Here's another tip. Run COFECHA again a few times, keeping the same segment length being tested (e.g., 50 years or 40 years), but decrease the amount of overlap in the segments. For example, I've found running COFECHA testing 40 year segments overlapped by 10 years (rather than the default 20 years) truly helps isolate problem areas!

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