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Contributed by Museum of Vertebrate Zoology, University of California, Berkeley.
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Transcription
Mayhew
1964
Journal
9.
Sept. 2 Glamis area, Imperial Co., Calif.
black sand does a short time
after the tide has receded. After
getting the needed information on Uma
notata and Urosaurus gracilisus
activity in September, we drove to
the eastern edge of the dunes
to get some soil temperature
measurements that the referee for
my Scaphiopus couchi paper felt
were needed. I dug a hole in the
sand under the dense shade of a
palo verde (Cercidium floridum) where
the shade was essentially permanent
(north side of tree). Then I
measured the soil temperature 50 cm.
beneath the surface, since this was
the deepest at which I found the
permanently moist layer. At the
same time, Al Bennett dug a
hole in the sand that was exposed
to the sun all day. This spot was
about 30 feet from my hole. We
measured the soil temperatures at the
same depths at the same time. The
readings were:
Shade Sun
30.8°C 34.9°C
At the time the air temperature
(1 meter) was 35.4°C. If the same
measurements had been made at