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here from Gruta del Palmito, Nuevo Leon, had previouslybeen known only from a single female specimen describedfrom Edinburgh, Texas. This species is represented byboth males and females in Gruta del Pa1mito and is hereredescribed. Both of these species are probablytrogloxenes. In addition, the troglobitic cirolanidisopod, Speociro1ana ~e1aezi, is reported from Sotanodel Arroyo, San Luis otosl.10. Vande1, A. 1965. flLes Trichoniscidae cavernicoles(Isopoda Terrestria: Crustacea) de l'Amerique du Nord."Anna1es de Speleologie, 20(3):347-389.In addition to new species described from Texas andeastern caves, new records are included for the Mexicanterrestrial isopods. Protrichoniscus bridgesi is reportedfor the first time from s6tano del Arroyo, Sotano de 1aTinaja, and Ventana Jabal!, San Luis Potosi.Protrichoniscus vi11a1obosi is partially redescribedand Is recorded for the first time from Cueva del Carb6n,San Mart!n, Veracruz.71The AMCS NEWSLETTER is published six times a year by theAssociation for Mexican Cave Studies, P.O. Box 7672 UniversityStation, Austin, Texas 78712. Membership in the AMCS is $5.00for the calendar year, with memberships starting at the firstof each year. Persons joining after the first of the year willreceive all publications for that year. Also, publications forthe year of 1965 are still available by writing to the AMCS.Members are urged to submit articles for publication. Thearticle may cover any phase of Mexican speleology. Trip reportsare requested from all trips.Editor•••••••••••••••••••.••• Terry W. RainesAssistant editor••••••••••••• John FishTreasurer•••••••••••••••••••• Philip Winsborough
THE ASSOCIATION FORMEXICAN CAVE STUDIESNEWSLETTERTRIP REPORTSXllitla, SoL.P.XlIIlla, SoL. Po; GuerreroCueva del Diablo, Sabinal Hidalgo, N. L.HISTOPLASMOSISPARQUE NACIONAL DE LA GRUTA DEL PALMITOTHE ORDER RICINULEI IN MEXICAN CAVESMEXICAN CAVE BIOLOGY: ANNOTATED BIBLIOGRAPHYVolume II Number 4 July . Augult 1966
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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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Page 24 and 25: Persons: Ed Alexander, Bob Burnett,
Page 26 and 27: go north of Galeana to Ranchero Sou
Page 28 and 29: 26Persons: Chip Carney and Don Eric
Page 30 and 31: =::::::?------------I.r-L6-\. MUD S
Page 32 and 33: Sandy-floored passage in S6tano de
Page 34 and 35: slopes, made difficult by the thin
Page 36 and 37: Persons: Faye Chapman I Jonathan Da
Page 38 and 39: a rutted road. On the other side of
Page 41 and 42: Entrance to S6tano de San Antonio.
Page 43 and 44: totENTRANCEo 30FEET60 90iCUEVA DETL
Page 45 and 46: contained a long, steep talus slope
Page 47 and 48: Entrance to Cueva del Salitre.Photo
Page 49 and 50: On July 12 I had an hour's intervie
Page 51 and 52: THE ASSOCIATION FORMEXICAN CAVE STU
Page 53 and 54: One of the many Santa Fe dirt sinks
Page 55 and 56: 330 feet. At the bottom along one s
Page 57 and 58: species of milliped of a group not
Page 59 and 60: secondary opening one-third of the
Page 61 and 62: After a perusal of our topo maps th
Page 64 and 65: HUAUTLA DE JIMENEZ, OAXACAAREA SKET
Page 66 and 67: 11. Pit just down hill from pit 10.
Page 68 and 69: 21. SOTANO DE SAN AGUSTIN - This s6
Page 70 and 71: LOWERENTRANC.EPROI="ILEuppeR£NTRAN
Page 72 and 73: RECENT PAPERS ON MEXICAN CAVE BIOLO
Page 76 and 77: THE ASSOCIATION FOR MEXICAN CAVE ST
Page 78 and 79: View north along valley of the Inte
Page 80 and 81: Typical fissure passages in S6tano
Page 82 and 83: valley below the resurgences were d
Page 84 and 85: point on, green mosses cover the wa
Page 86 and 87: Persons: John Fish, David McKenzie,
Page 88 and 89: Buena la dozen eager guides led us
Page 90 and 91: los Riscos (see sketch map on page
Page 92 and 93: Persons: Jim and Barbara Hershberge
Page 94 and 95: 20' PITENTRANCE L-l. ", ...,\ '-'-~
Page 96 and 97: Editor's Note: The following propos
Page 98 and 99: permanent river in the area is the
Page 100 and 101: Develop the cavern and an access to
Page 102 and 103: OF THEPROPOSEDPARQUE NACIONAL DE LA
Page 104 and 105: 100area, was rather surprising, sin
Page 106 and 107: 1.2.3.4.5.6.MEXICAN CAVE BIOLOGY:AN
Page 108 and 109: 15.16.17.18.19.Reddell" James R. 19
Page 110 and 111: THE ASSOCIATION FORMEXICAN CAVE STU
Page 112 and 113: 107NEWSNOTESTABLE OF CONTENTSTRIP R
Page 114 and 115: 109CAVEMAPSDuring the past six year
Page 116 and 117: 111CAVES OF GUERRERO AND MORELOSJOH
Page 118 and 119: 113in the volcanic detrital deposit
Page 120 and 121: 115CAVE DESCRIPTIONSGRUTA DE ACUITL
Page 122 and 123: 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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NENCINO - JULILO ROADSSOTANO DE SAN
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FEETo100SOTANO DE LA JOYAJOYA DE SA
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137had not been checked was followe
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139a high mountain karst area with
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-SaltilloMonter..SKETCHMAPofCA~ON D
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143another 15 miles before we turne
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ENTRANCE Q~\\F~\~.~ ..~~-.~~~O~v'\.
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147S6tano de las Ra!ces lon the sam
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149and color motion pictures. The f
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151ground in the area. (See photogr
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ENTI'ANCEGRUTADENAVIDADMUNICIPIO DE
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155NOTES ON THE EXPLORATION OF SOTA
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157obtain a rough idea of how many
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159Grutas de Mogote, located one mi
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161Past the first large room (appro
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163-749 feet. The left-hand passage
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165it looked a good 300 feet deep.
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167was. Almost 2 hours were require
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Haarr, Allan P. 50 Clover Dr Delmon
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171Young, sam and Diane 474 lOth Av
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173RECENT ADDITIONS TO THE KNOWLEDG
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175large horizontal passage about 1
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177S6tano de Huitzmolotitla, with a
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AreaNorth ofMonterreySouth ofMonter
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182BIOLOGYSECTIONMEXICAN CAVE BEETL
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184from Canada to Oaxaca, but only
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INDEXVOLUME1966II
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187Cantabroniscus primitivus isopod
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189Hooton, Diana 6:149-154Hosley, B
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191pictographs 5:121Pinal de Amo1es
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193from La Si11eta looking eas~)f.
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17MB PDF - Association for Mexican Cave Studies

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