183(depigmented)1 and has the eyes reduced to tinYI pale spots.About 15 specimens have been collected in 25 yearsl apparentlyall of them from or quite near the entrance room of the cave.Two additional species of Mexaphaeno~sl not yet describedlhave been discovered by John Fish in the6tano de TeJamanil (Qro.)and in a small cave in Valle de los Fantasmos (S.L.P.). The occurrenceof all three of these species in caves at relatively highelevations is noteworthy. There is considerable evidence that thetroglobitic trechines of Europe and the United States are descendantsof boreal <strong>for</strong>est species which were widespread during periodsof glacial advance during the Pleistocenel but were able to survivethe warm, dry climate of the interglacials only by retreating intocaves where they underwent regressive evolutionary modificationsincidental to adaptation to the cave environment. Absence of troglobitictrechines (and troglobites of most other groups whichlive in humus and moss carpets) from tropical regions is attributedto the "isothermal" climatic conditions of the tropics. In otherwordS,. there were no major climatic changes which changed the surface(SOil and moss) environment to such an extent that surfacemembers of troglophUe species became extinct and the cave popUlationsthus became isolated in caves and developed into troglobites.The climate of Mexico, particularly the northern portions and thehigher elevations, was certainly much colder and wetter duringglacial maxima than it is today. It will be most surprising if aspecies of Mexaphaenops turns up outside of a high mountainousregion.In European trechinesl Jeannel was able to point to gradedseries of species which probably illustrate the stages from a surfacespecies (eyes, wings, pigment) to a cave species (troglobite).In the genus Duvalius, particularly, there are species which liveunder stones in the mountains and have small eyes, often elongatebody parts, and reduced pigment. There are even eyeless specieswhich live deep in humus in the mountains and resemble cave species.Bolivar's earlier discovery of Paratrechus sylvaticus, a pale, depigmentedspecies with small eyes, in Morelos and Distrito Federal,seem to provide a "missing link" in the construction of the samesort of ~raded series between typical Paratrechus and Mexaphaenopsprietoi s lAnales Esc. Cien. BioI., 2: 111-1181 pl. 9, 1941). P.1vaticus was p1aced-rn-a new-subgenus, ~grOdUValius, but tned1agnostic characters which Bolivar cited n 1941 have since beencalled into question by the description of other Paratrechus spp.,and it is now doubtful that P. sylvaticus is distinct enough towarrant subgeneric separation from other Paratrechus. The latest"link" in the series was <strong>for</strong>ged with the discovery of a blinds2ecies of Paratrechusl closely related to P. h!lvaticus, in thes3tano de Tejamani1 (Qro.) by John Fish. r:n t s species, stillundescribed, the eyes are very small, palel and non-functional,but the body parts are not slender and elongate as in Mexaphaenops.It seems likely that Mexaphae~s includes the relicts or a mucholder invasion of the caves t this newly descovered species ofParatrechus. For the future, the biological exploration of <strong>Mexican</strong>caves at the higher elevations should prove most interestingl particularlyas additional species of troglobitic trechines show up.The agonine carabids include the genera Rhadine and Mexisphodrus,as well as Agonuml ClIE~~isl and a few other genera collectedrn-<strong>Mexican</strong> caves. No trog 0 c Rhadine have been found in Mexico.The genus is rather widely distributed in Western North America,
184from Canada to Oaxaca, but only 3 species are known east of theGreat Plains. Species of Rhadine have a predilection <strong>for</strong> cool,dark habitats, and they are consequently found in mammal burrows,caves, cellars, and similar places. Some species (including R.euprepes from Mexico) live in <strong>for</strong>ests, under rocks and logs. -Onlyone species group (the subterranea group) contains real troglobites,and these species are restricted to central Texas.Mexisphodrus, described as a new genus by Barr (Coleopt. Bull.,19:. 6s=72~ 1965), was first discovered in the s6tano del Profesor(Veracruz) by Terry Raines and Bill Bell. Additional species havebeen taken in a small cave at Jacala (Hidalgo) (Hendrichs andBOlivar~ 1966; Ciencia, 25: 7-10, pl. 1); the s6tano de Tlamaya(S.L.P.); and in the Sotano de la Joya de Salas and a small sinkholeat Rancho del Cielo (Tamps.) (Barr, 1966. ps~che, 73: 112-115).M. veraecrucis Barr and M. profundus Barr appear 0 be incipienttroglobites; they are wingless and depigmented and have very small,pale eyes. M. tlamaEfaensis Barr is a winged species with largeeyes, and ~.-gertsc Hendr. & Bol. is somewhat intermediate, stillretaining moderately well-developed eyes and a fairly dark pigmentation.Three undescribed species of the apparent troglobitevariety have been recently collected in Queretaro (s6tano de Camposantos,Cueva de las Tablas), San Luis Potosi (Valle de losFantasmos), and Oaxaca (S6tano de San Agustin).The special interest in Mexisphodrus derives from the factthat, until 1957, agonines belonging to the group of "true sphodrinesl1were known only from the Old World, ranging from theCanary Islands across the Mediterranean region into China. In1957 Straneo (Ciencia, 17: 81-84) describes the <strong>Mexican</strong> genusBo1ivaridius from surface material, suggesting that species ofthis genus belonged with the true sphodrines, despite lack of certaindiagnostic characters found in the European genera but not inthe <strong>Mexican</strong> one. Prosphodrus was described from New Zealand byBritton in 1959 (Proc. Entomo1. Soc. London (B), 28: 103-106)j P.wa1toni is a cave <strong>for</strong>m (dark, with eyes) which, like Bolivaridius,appears to be a primitive sphodrine. The characters and generalbody <strong>for</strong>m of Mexis1hodrus much more clearly suggest relationshipto the true sphodr nes than do those of Bo1ivaridius, but bothgenera are, in effect, ltmissing links" that make it difficult todraw arbitrary lines of classification and say what is a sphodrineand what is not. Other sphodrines inhabit Gruta del Pa1mito(N.L.), Cueva de 1a Boca (N.L.), and Texas caves of the Del Rioregion; these may constitute a third genus of North Americansphodrines, but their study has not yet been completed.The collection 1n November, 1966, of an eyeless, apparentlytroglobitic carabid of the tribe Scarit1ni, in the Sotano de laJoya de Salas, by Orion Knox and El Alexander, has added a remarkablenew element to the growing troglobitic fauna of Mexico.Scaritines, which include small to medium-sized, narrow-ltwaisted ltbeetles which burrow in gravel at the edge of streams, have only2 known trog1obit1c species--one in Yugoslavia and one in Italy-both of which are apparently descended from hum1co1ous ancestorsand both of which, by evolutionary convergence, superficially resemblecave trechines. The Tamau1ipas cave scaritine, about 6.5 mmin length, 1s very different in appearance, although it, too, isrelatively slender and depigmented and without eyes. The bestguess that one can make at the present time is that this insect is
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THE ASSOCIATION FORMEXICAN CAVE STU
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de T1amaya the deepest surveyed cav
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and is about 200 feet long. It is p
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Modesto G6mez Saldivar, 1898-1966Mo
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JOHN WILLIAM FRANCIS HARRISONBORN B
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have been found even at Harrison's
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Note: This is the first of a series
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it has rained three and four inches
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The Deep Caves or the Western Hemis
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Persons: Ed Alexander, Bob Burnett,
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go north of Galeana to Ranchero Sou
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26Persons: Chip Carney and Don Eric
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=::::::?------------I.r-L6-\. MUD S
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Sandy-floored passage in S6tano de
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slopes, made difficult by the thin
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Persons: Faye Chapman I Jonathan Da
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a rutted road. On the other side of
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Entrance to S6tano de San Antonio.
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totENTRANCEo 30FEET60 90iCUEVA DETL
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contained a long, steep talus slope
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Entrance to Cueva del Salitre.Photo
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On July 12 I had an hour's intervie
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One of the many Santa Fe dirt sinks
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330 feet. At the bottom along one s
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species of milliped of a group not
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secondary opening one-third of the
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After a perusal of our topo maps th
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HUAUTLA DE JIMENEZ, OAXACAAREA SKET
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11. Pit just down hill from pit 10.
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21. SOTANO DE SAN AGUSTIN - This s6
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LOWERENTRANC.EPROI="ILEuppeR£NTRAN
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RECENT PAPERS ON MEXICAN CAVE BIOLO
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here from Gruta del Palmito, Nuevo
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THE ASSOCIATION FOR MEXICAN CAVE ST
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View north along valley of the Inte
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Typical fissure passages in S6tano
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valley below the resurgences were d
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point on, green mosses cover the wa
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Persons: John Fish, David McKenzie,
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Buena la dozen eager guides led us
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los Riscos (see sketch map on page
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Persons: Jim and Barbara Hershberge
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20' PITENTRANCE L-l. ", ...,\ '-'-~
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Editor's Note: The following propos
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permanent river in the area is the
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Develop the cavern and an access to
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OF THEPROPOSEDPARQUE NACIONAL DE LA
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100area, was rather surprising, sin
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1.2.3.4.5.6.MEXICAN CAVE BIOLOGY:AN
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15.16.17.18.19.Reddell" James R. 19
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107NEWSNOTESTABLE OF CONTENTSTRIP R
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109CAVEMAPSDuring the past six year
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111CAVES OF GUERRERO AND MORELOSJOH
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113in the volcanic detrital deposit
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115CAVE DESCRIPTIONSGRUTA DE ACUITL
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117CUEVA DE CARLOS PACHECOcavecavec
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119CUEVA DEL DIABLOLocation:Descrip
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121References:levels. The entrance
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123decorated passage which extends
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125collections by Stanley Kiem (Loo
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1279.10.11.12.13.14.caves or cave-l
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131TABLE OF CONTENTSNEWS NOTES. ...
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- Page 144 and 145: 137had not been checked was followe
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- Page 150 and 151: 143another 15 miles before we turne
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- Page 154 and 155: 147S6tano de las Ra!ces lon the sam
- Page 156 and 157: 149and color motion pictures. The f
- Page 158 and 159: 151ground in the area. (See photogr
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- Page 162 and 163: 155NOTES ON THE EXPLORATION OF SOTA
- Page 164 and 165: 157obtain a rough idea of how many
- Page 166 and 167: 159Grutas de Mogote, located one mi
- Page 168 and 169: 161Past the first large room (appro
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- Page 172 and 173: 165it looked a good 300 feet deep.
- Page 174 and 175: 167was. Almost 2 hours were require
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- Page 178 and 179: 171Young, sam and Diane 474 lOth Av
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- Page 182 and 183: 175large horizontal passage about 1
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- Page 198 and 199: 189Hooton, Diana 6:149-154Hosley, B
- Page 200 and 201: 191pictographs 5:121Pinal de Amo1es
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