Tag-Archive for » dendrochronology «

January 14th, 2009 | Author: sarcozona
getting a cookie

My mentor, cutting down a dead tree for me

I want to know how different soil types affect pinyon pine growth during drought and if there’s a difference in growth between trees that die in the drought and those that have survived so far.  So I needed some cookies.

tree cookies

tree cookies

We had no idea that there would be two feet of snow on the ground at the site, which made working much much harder.  As much as I usually hate fieldwork, you would think that I would have had a terrible time.  Actually, I had a great time.  Of course, that might have had a little to do with the drugs I had to take to deal with the change in elevation.

May 28th, 2008 | Author: sarcozona

ResearchBlogging.org

Carbon dioxide levels have been increasing since the industrial revolution and have been increasing really really fast since the 1950s. You’ve all seen the hockey stick graph.

hockey stick graph

I’ve been looking at pinyon pine tree rings for the past year and think there might be something going on with increasing CO2 and what the rings are doing. So I’ve got a stack of papers to read through and thought I’d share some of them with all of you.

Carbon dioxide is pretty good for plants because plants need carbon for photosynthesis. We’re interested in what higher levels of CO2 will do to plants because if plants are growing more and eating more carbon dioxide it could help slow down global warming. But giving most plants most places extra carbon dioxide doesn’t seem to do much in the long run because plants need lots of other things to grow, like nitrogen and water, and carbon isn’t usually the most limiting. It’s the same for you: it doesn’t matter how many vegetables you eat if there’s no water.

But what about plants where carbon might be a limiting factor for growth? Carbon can be limiting in hot, dry places because to get carbon, plants have to lose water. Plants have little tiny pores in their leaves called stomata. They have to open these to let in CO2, but water escapes whenever they’re open. A lot of plants that live in hot, dry places have evolved a different kind of photosynthesis to deal with this.

stoma

Another place carbon might be limiting is at very high elevations. Atmospheric CO2 concentrations decrease with increasing elevation. That means that in the same amount of space there’s less CO2. This happens to all gases. Flagstaff is above 2000 meters. When people move here, they have a hard time breathing for awhile because of the lower oxygen concentration.

Lamarche et al. looked at tree rings in the 1980s of bristlecone pine growing at 3100 meters. They found that the trees had increasing growth since about 1840. Initially they thought that this was due to warmer temperatures, but then when it cooled down in the 60s, the trend kept going and even accelerated. So, the faster growth wasn’t due to hotter temperatures.

bristlecone

But was it caused by higher CO2 levels? Plants can only use so much CO2, no matter how much is available. Like at Thanksgiving dinner, there’s lots of food available, but you can only eat so much. In the 1960s, CO2 was between 223 and 230 ppm at 3500 meters. For spruce, that concentration is well below what it considers CO2 saturation and so is probably well below what bristlecone considers saturation.

While the authors didn’t really have enough data from enough places to say for sure CO2 makes trees growing at high altitudes grow more, what they do have certainly suggests it.

This paper is over 20 years old, so we’ll see what more recent papers have found…

LAMARCHE, V.C., GRAYBILL, D.A., FRITTS, H.C., ROSE, M.R. (1984). Increasing Atmospheric Carbon Dioxide: Tree Ring Evidence for Growth Enhancement in Natural Vegetation. Science, 225(4666), 1019-1021. DOI: 10.1126/science.225.4666.1019

January 07th, 2008 | Author: sarcozona

I use a program called COFECHA to help crossdate trees. COFECHA uses some old school formats developed for punch-cards. Excel, which I used to make changes to ring widths, does not like these formats. There are lots of programs for changing formats, but it’s all a bit confusing.

Many dendrochronology programs produce and use Compact/Precision formats. When crossdating trees with the program COFECHA, it is often useful to convert Compact/Precision formats to formats recognized by spreadsheet programs like Excel and then convert back to Compact/Precision formats to run through COFECHA. So for any other confused dendrochronologists out there, here’s a method that works for me.

Compact/Precision format looks like this when you open it with notepad:

ira 11946 170 200 216 755

ira 11950 529 332 405 342 384 760 647 363 556 466

ira 11960 288 431 490 124 827 282 319 248 441 1082

ira 11970 1601 498 992 1407 850 1053 1356 951 1145 1621

ira 11980 1756 1381 1397 1626 1868 2739 2447 2250 1684 1942

ira 11990 1401 1390 861 1389 1158 1421 1454 1040 -9999

Sometimes the numbers seem to run together, but each line will start with a series identifier and each series will end with -9999.

Convert file from Compact/Precision to tab delimited .txt file with program YUX. Open .txt file with Excel and make necessary changes, being sure to save as a tab delimited .txt file. Convert to Compact/Precision format with program CASE, being sure to save the new file as a .rwl. COFECHA should be able to read this file.

If you get COFECHA output that only includes the title or part of the desired output, try playing around with the print options in COFECHA.  If COFECHA produces a completely empty output file, try copying and pasting the information from your .rwl file into an existing .rwl file and saving it as a new .rwl file.

All programs can be downloaded from the Ultimate Tree Ring Web Pages run by Henri Grissino-Mayer.

tree rings