xt79zw18nk61 https://exploreuk.uky.edu/dips/xt79zw18nk61/data/mets.xml Alabama Alabama Museum of Natural History 1931 Other titles include: Alabama Museum of Natural History museum paper, Geological Survey of Alabama, Museum of the Geological Survey of Alabama. Other creators include: United States. Work Projects Administration, Geological Survey of Alabama, Tennessee Valley Authority. Issues for 1, 3 carry no series numbering. No. 2 also as Education papers no. 1. UK holds archival copy for ASERL Collaborative Federal Depository Program libraries. Call number  AS36 .A2. journals  English University, Ala. : Alabama Museum of Natural History, 1910-1960 This digital resource may be freely searched and displayed in accordance with U. S. copyright laws. Alabama Works Progress Administration Publications Museum Paper, no. 12, 1931 - including "Alabama Museum of Natural History" by T.H. Aldrich, D.Sc. text Museum Paper, no. 12, 1931 - including "Alabama Museum of Natural History" by T.H. Aldrich, D.Sc. 1931 1931 2015 true xt79zw18nk61 section xt79zw18nk61       V  
     
  .}c0l0g1cal Survey 0{Alabama ¢  
 A WALTER BRYAN ]ONES, State Geologist    
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DESCRIPTION OF A FEW ALABAMA EOCENE IQI - ~  
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SPECIES AND REMARKS ON VARIETIES   - . { I
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it   DESCRIPTIONS OF SPECIES tp thickness Of
( These species are all from the collection of the "Alabama   connected w
it W Museum of Natural History," and the types are in this Museum.   Rcmmlx
I I V I ?.; Q. ments at Bl:
i   I Lerjfusus pagoda, Heilpr. This form is figured from one like . gogligifoégi
  M the type which is figured in Vol. 3, in Professor Harris’s Bulle- jp. _
{ ( tin, Plate 6, fig. 10, pp 51. Professor Heilprin just gives the 10- { Ailmfb
; {   cation as Eocene of Alabama; it probably is from Wood’s Bluff t Of the interl
j ` l Horizon. There are a great many varieties of this form as stat- g D1"- H- G- S‘
j     ed by Professor Harris. It remains for the Nanafalia Beds to   may 1931, 3
9 - i show stout shells like L. indentus, Harris, (pl.5 fig. 5) and other N Lggaljt
W `i { forms almost without spines, (pl. 5. fig. 1) from Wood’s Bluff iii State Get-,10,
t Alabama; forms with a single row of spines (pl. 5, fig. 2 and 3) ;   Ot (jtttjbom.
Q forms with a double row of spines, (pl. 5 figs. 6 and 7) ; and an- i jlay in the I
  other with a triple row of spines on the body whorl (pl. 5 fig. 8). ] tO1~y_"
ii { It is hardly necessary to give names to these varieties but they 2  
 I all belong close to the parent. (pl. 5 fig 7.) represents Levifusus 2 Lgmmt
    supraplanus, Harris which seems to be a variety also. T Omamgnted
 Q, I _ nearly equa
“ Volutilzthes petrosus, Con., occasionally this species which is Q Cana] aye 5
It \ common in Claiborne occurs with a double row of spines on the i sugy tytmg
/7 body Wh01‘l. (pl. 6 fig. 3). `_ broadly ov;
‘i` . Crrzssatcllites (lf(l€fO7‘77ZZ.S, Con., var., a single form l1101`€   upper part
Ii nearly like the Maryland form was found in the Gosport Bluff I2 m‘m‘ (D
, _ or Claiborne horizon and differs greatly from the ordinary Clai- F Localil
Jl , borne species, (pl. 6 fig. 5). It may possibly be a very sulcate c collected th
I; I form of C. p2·oi‘c.rfa. Some of that species are also sulcate. I to Lcrifusv
  i ( Eufrcp}2occ2·a.s haltomz', n. sp., shell nautiloid in appearance. » ""‘k‘§,t1;¥f
    (pl. 1 fig. 1). Substance of our shell thin, shell large, the i the Cljgboi
gi I ) greatest width being 240 m.m. reduced to 140 m.m. in the ph0-   Comhg iq
  .   tograph, sutures (pl. 3 fig. 2) rather straight but turning into   it bwt tok
. the umbillicus abruptly having an acute angle. The SQDIEH RFQ §° `
  Y flat. The outer chamber seems to have been large. Sutul‘€S E Arca-
f   are rather close together. (Pl. 3 Hg. 3) is another view show-   1A). Pro
l?

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ing the sutures. The siphuncle is small, round and high up on   . [T  
the septa, pl. 3 fig. 3). (Pl. 2 fig. 1) shows the thickness of the     — P   i
specimen looking down on the top. The light part shows the   _ A j ; 
thickness of the shell and the darker part is part of the shell   n . .  
Jama connected with the base. . Qi    .    
Bum Remarks: This species is very common but mostly in frag-        
s ments at Black Bluff, Tombigbee River, Alabama, or the Sucar-  T     l.  
3 mw nochee formation. It is named after the discoverer, William L.   S. »    
;uH€— Haltom, Curator of this Museum.      
IQ 10- Atm·ia alolmnzcnsis, Morton, (pl. 4 fig. 1). This is a cast l_      
Bluff of the interior of this species and has already been published by ‘ i      
gmt- -» Dr. H. G. Schenck, in Vol. 19, number 19, University of Califor—   V4  
ds (O nia, 1931, and is repeated herewith.     ‘    
3th€1` Locality: The specimen was found by Dr. E. A. Smith, late F   .  
Bluff State Geologist, in the Upper part of the Jackson horizon, west     li  
?l 3) 9 of Claiborne a few miles. There is another specimen quite sim- l it   A C lili  
Cl 8]* ilar in the collection of the "Alabama Museum of Natural His-      
¥· Sl tory."     A A 1;-  
they   g; _ ?
mgm Lcz·ifcu.s2z.s l>i.spz“noxus, n. sp., shell medium, whorls 6 or more, A F; ‘  
ornamented on the body of the whorl with two rows of spines E   _ s  
_ nearly equal in size and 12 in each row. Both the spire and the     l *  
Ich is canal are somewhat damaged. The surface is covered with     *_  
H the finely transverse lines becoming coarser on the canal. Aperture   gl V    
broadly ovate, outer lip striated within. A thin callus on the .·        
more upper part of the inner lip. Length remaining 28 m.m. width   , .i`-    
Bluff 12 m.m. (pl. 5 fig. 4). if (   if  
Clai- Locality: Tuscahoma Landing, Alabama. Dr. E. A. Smith. `     4 A V;  
ilcate collected this form a number of years ago and considers it equal        
to Lcri_f1¢sn.s firm/zncri, Harris. Its locality and other characters [V   ~'  
ance' makes this species probably an ancestor of the Jackson form.   J ~ {__  
the Omfzlrcnus rllscoiclalis, Con. This species is very rare in   ‘  
’phO_ U the Claiborne sand at Claiborne, Alabama. The figure given by   `if  
_ mm Conrad is poor and Mrs. Katherine Palmer of Cornell thought 5      
  are it best to refigure the same. See (pl. 6 figs. 4 & 4A).      
tures Arca. cnculloidcs, Con., this is figured on (pl. 6 figs. 1 &     l`    
;ho‘.v— V 1A). Professor Harris has stated that it is very doubtful that   `.      
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    this species is found in the Claiborne sand bed but this Survey _E’i`”’U“”
{   has two or three fine specimens that undoubtedly came from Clijubome Sa]
ZA Y Claiborne. The drawings have been presented to the Survey - bemg more Q
{ by Professor Harris of Cornell. .
i , Pseudolira ozanafaliacizsis, n. sp. shell rather large, smooth,
il l ovate, subglobose, suture distinct; body whorl slightly con- g.
I     ‘ l stricted close to suture expanding rather quickly. A line on `
» ; 1   upper half of same indicates the position of a small tooth on the  
i   Q outer lip. Surface of body whorl is marked with fine transverse ‘
{ lines, thickened callosity near junction of the upper and outer T
_ g i lip. The interior is filled with natrix in this specimen. Length
j   i 60 m.m. breadth 38 m.m. ·
· ii i Locality: Nanafalia Beds, Tombigbee River, Alabama.  
.   ’   Rcnmrles: This shell varies from the common Pseuclolira A
i   l wfustcz, Con., in the shape of the spiral whorls the position of .
      the tooth and there are varieties connecting this species with `
, I l ( some at Claiborne, Alabama. The shape of the aperture seems y
il l to connect it with Aincilla. (pl. 1 fig. 2). _
if ii Fusus rcgularoicles, n. sp. Shell regularly fusiform, spire
it 1 high, suture wavy; whorls seven, without the embryonic ones `
 ‘ l which are missing. A broad space between the suture carrying
 ; some transverse and vertical raised lines; angulated above the `
%\ l suture with about 8 or 10 nodes and 2 or 3 revolving raised .‘
  , lines. Body whorls with strongly raised transverse lines to tip
.1}. `   of canal. Aperture ovate, smooth within, a callus on the inner T
ii   lip; canal long with strong raised lines down to the tip. Length
g 50 m.m. width of body whorl 18 m.m. (pl. 5 fig. 9). ·
  Remarks: This shell is strongly marked but approaches .
  Lczifusus.
  A   Locuhty: W. D. Matthews Landing, Alabama. ·
  ( Fusus nzohri, Aldr., it seems as if Harris’s shell named by {
gil   him as Fusus bellamzs is the same as the above. My specimen W35 fe
  .   described from a half grown shell but fragments connect thi? ‘
  it two. The original type is in the collection of Johns Hopkins
if T University, together with another specimen showing a connec- V
li I   tion to Harris’s form as named as above.  
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Yogi Claiborne sand at Claiborne. Differs from the E. Iigvzitica by  jill      
We`, being more elongated and highly polished.     _ ;
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g pi Figures of various species and varieties.
i 5 Fig. 1. Levifusus pagoda, Heilpr.
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; }· Fig. 3. Probably the type specimen.  
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;'_ Fig. 5. Levifusus indentus, Harris. .i
i l Fig. 6. Levifusus pagoda. Heilpr with a double row of l
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  . Fig. 8. Levifusus pagoda var. with a triple row of spines.
i' e Fig. 9. Levifusus regulariodes n. sp. ~ in
     
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