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Early in 1960 an unusual opportunity arose to carry on biological field
work in the midst of virgin rainforest in southern El Petén, Guatemala.
At that time the Ohio Oil Company of Guatemala had an air strip and camp
at Chinajá, from which place the company was constructing a road
northward through the forest. In mid-February, 1960, J. Knox Jones, Jr.
and I flew into El Petén to collect and study mammals, reptiles, and
amphibians. While enjoying the comforts of the fine field camp at
Chinajá, we worked in the surrounding forest and availed ourselves of
the opportunity to be on hand when the road crews were cutting the tall
trees in the forest, thereby bringing to the ground many interesting
specimens of the arboreal fauna. We stayed at Chinajá until late March,
with the exception of a week spent at Toocog, another camp of the Ohio
Oil Company located 15 kilometers southeast of La Libertad and on the
edge of the savanna. Thus, at Toocog we were able to work both in the
forest and on the savanna. In the summer of 1960, John Wellman
accompanied me to El Petén for two weeks in June and July. Most of our
time was spent at Chinajá, but a few days were spent at Toocog and other
localities in south-central El Petén.
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A tremendous lowland area stretches northward for about 700
kilometers from the highlands of Guatemala to the Gulf of Mexico. The
northern -thirds of this low undeniable is bordered on 3 aspects with the aid of using seas
and bureaucracy the Yucatán Peninsula. The lowlands at the bottom of the
Yucatán Peninsula make up the Departamento El Petén of Guatemala. The
region with which this file is worried includes the south-valuable
a part of El Petén.
Physiography
Immediately south of Chinajá is various hills, the Serrania de
Chinajá, having an nearly due east-west axis and a crest of approximately 600
meters above sea level. South of the Serrania de Chinajá are
succeedingly better ridges constructing as much as the Meseta de Cobán and Sierra
de Pocolha and sooner or later to the principle Guatemalan highlands. The northern
face of the Serrania de Chinajá is a fault scarp losing all at once from
approximately 650 meters on the crest to approximately a hundred and forty meters at the bottom. From the
base of the Serrania de Chinajá northward to the Río de los angeles Pasión at
Sayaxché the terrain is lightly rolling and has a complete comfort of approximately
50 meters. North of the Río de los angeles Pasión is a low dome attaining an
elevation of one hundred seventy meters at La Libertad; see Stuart (1935:12) for further
dialogue of the physiography of valuable El Petén. The rocks in
southern El Petén are predominately Miocene marine limestones; there are
occasional wallet of Pliocene deposits. There is little proof of
subterranean answer at Chinajá, however northward in valuable El Petén
karsting is not unusualplace. The higher few inches of soil is humus wealthy in
natural matter; beneath that is clay.
Climate
The weather of El Petén is tropical with equable temperatures for the duration of
the year. Temperatures at Chinajá various among a night time-time low of 65°
F. and a sunlight hours excessive of ninety one° F. at some point of the time of our visits. In the
Köppen machine of class the weather at Chinajá and Toocog is Af.
Rain falls for the duration of the year, however there may be a great dry season. To
every body who has traveled from south to north in El Petén and the Yucatán
Peninsula, it's far apparent from the adjustments in flowers that there may be a
lower in rainfall from south to north. There is a great
distinction among Chinajá and Toocog. Although rainfall facts aren't
to be had for Chinajá and Toocog, there are facts for close by stations
(Sapper, 1932). At Paso Caballos at the Río San Pedro approximately forty
kilometers northwest of Toocog the common annual rainfall quantities to
1620 mm.; the driest month is March (21 mm.), and the wettest months are
June (269 mm.) and September (265 mm.). At Cubilquitz, Alta Verapaz,
approximately 35 kilometers south-southwest of Chinajá and at an elevation of
three hundred meters, the common annual rainfall is 4006 mm.; the driest month is
March (128 mm.), and the wettest months are July (488 mm.) and October
(634 mm.).
During the 18 days in February and March, 1960, that we saved facts on
the climate at Chinajá slight to heavy showers took place on seven days.
During our live there in June and July rain fell each day, because it did in
Toocog. However, at some point of the week spent at Toocog in March no rain fell.
Vegetation
The flowers of northern and valuable El Petén has been studied with the aid of using
Lundell (1937), who made best passing feedback regarding the flowers of
the southern a part of El Petén. No floristic research had been made
there. The following feedback are always short and are intended
best to present the reader a trendy photo of the woodland. I actually have covered
names of most of the commoner bushes that I recognized.
Chinajá is placed in a tremendous expanse of unbroken rainforest. In this
woodland there may be a great stratification of the flowers. Three
strata are apparent; withinside the uppermost layer the tops of the bushes are
from forty to 50 meters above the floor. The spreading crowns of the bushes
and the interlacing vines shape a almost non-stop cover over the decrease
layers. Among the not unusualplace bushes withinside the higher stratum are _Calophyllum
brasiliense_, _Castilla elastica_, _Cedrela mexicana_, _Ceiba
pentandra_, _Didalium guianense_, _Ficus_ sp., _Sideroxylon lundelli_,
_Swietenia macrophylla_, and _Vitex_ sp. (Pl. 1, fig. 1). The center
layer of bushes have crowns approximately 25 meters above the floor; those bushes
in a few locations wherein the higher cover is lacking shape the tallest bushes
withinside the woodland. This is specifically actual on steep hillsides. Common bushes
withinside the center layer consist of _Achras zapote_, _Bombax ellipticum_,
_Cecropia mexicana_, _Orbignya cohune_, and _Sabal_ sp. The lowermost
layer reaches a top of approximately 10 meters; in lots of locations withinside the woodland
this accretion is absent. Common bushes withinside the decrease stratum consist of
_Crysophila argentea_, _Cymbopetalum penduliflorum_, _Casearia_ sp., and
_Hasseltia dioica_.
The floor cowl is sparce; reputedly only some small herbs and ferns
stay at the closely shaded woodland ground. Important herpetological
habitats consist of the leaf muddle, rotting stumps, and rotting tree
trunks at the woodland ground and the buttresses of among the gigantic
bushes, specifically _Ceiba pentandra_ (Pl. 2). Epiphytes, specifically
diverse forms of bromeliads, are not unusualplace. Most often those are in
the bushes withinside the higher and center strata.
At Toocog there may be sharp wreck among savanna and woodland (Pl. 7, fig.
