DAVIDSON — SCOTTISH CARBONIFEUOUS llRACIIIOrODA. 
259 
SCOTTISH COUNTIES IN WHICH THE FOLLOWING CAEBONIFEROUS 
BRACHIOPODA HAVE BEEN DISCOVERED* 
Geneka and Species. 
anarkshire. 
6 
6 
■i 
Cfi 
bartonshire. 
•| 
bo 
a 
friesshire. 
leshii'e. 
burghshire. 
6 
0 
be 
.a 
lingtonshire. 
hire. 
'ickshii-e. 
o 
O 
<u 
1 
1 
m 
)£ 
u 
0 
M 
R 
P 
P-i 
w 
PQ 
1. T&rGbTcituld licistdtci' Sow... 
+ 
-f- 

+ 

+ 
2, . sctccuTus^ Martin . 
-|- 
4. 
4. 
3. vcsiculuTts. dc Koii 
4_ 
4. SpivifcTCi cluj)licicost(ij Phil. 
+ 
4- 
4- 
+ 
4- 
+ 
5. hisulcata, Sowerby . 
-1- 
4- 
+ 
4- 
_ trigonalis, Sowerby 
-l- 
+ 
-1- 
4- 
+ 
4- 
+ 
+ 
+ 
7. — ovalis, Phillips 
-f 
4- 
+ 
8. • piufjuiSy SowGrby... 
+ ? 
9 glcibi'dy Martin 
+ 
4- 
10. ■ Urii, Fleming 
+ 
4- 
4- 
+ 
+ 
11. — CctTluki€nsiSj Dav. .. 
+ 
12. lineatcij Martin 
+ 
+ 
+ 
+ 
4- 
4- 
4- 
13. SpiTifcTinci ct'istato.'^ var. oc- 
top I i cdtct' Sowerby 
4- 
4- 
4- 
+ 
4_ 
+ 
14. insculptctj Phillips 
+ 
1^5. layninosa, M'Coy 
16. A-tKyvis cuYi^hicjuo., Sowerby 
+ 
+ 
+ 
+ 
4- 
+ 
4- 
+ 
+ 
+ 
jjZci'jio-suZf'afci', Phil 
+ 
-j- 
4- 
+ 
4- 
+ 
18. RoyssiyVEveUle .. 
+ 
+ 
+ 
4- 
+ 
+ 
+ 
19. Retzia radialis, Phillips . . 
+ 
+ 
20. miyiiclwiicllci pufjiitiSy Mar 
+ 
+ 
4- 
+ 
+ 
21 . pleuy'od.oTij Phil 
+ 
4- 
+ 
4- 
+ 
+ 
+ 
+ 
+ 
22. Cdi^io.ToplioT'iob CTiLw ci\o Sow 
4- 
23. Stvoplium c7ici Tliowhoi (XoXis 
var. diiologoj and distoTtc 
Sowerby 
+ 
4- 
+ 
24. Bi^'eptorhynclms crenistria 
Phillips, and var. rad/ialii 
and var. Kellii 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
25. Orthis resxpinatay MaHiH" 
+ 
-f- 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
26. Michelini, I'Eveille .. 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
+ 
27. Chonetcs Hdrdrensis, Phil. 
+ 
+ 
+ 
+ 
-r 
+ 
+ 
+ 
28. Buchidridy de Kon. 
+ 
29. Productus gigdnteiis^ Martin 
+ 
+ 
+ 
(- 
+ 
+ 
+ 
+ 
+ 
30. latissimus, J. Sow 
+ 
+ 
+ 
+ 
+ 
31. cordj d'Orbigny.. 
+ 
+ 
+ 
+ 
+ 
* This Table shows the Shh-cs in which Carboniferous strata exist, as well as the amount of 
work done in the way of collecting organic remains. Those counties from wliich few species 
are recorded wiU no doubt upon fuller exploration be IV.und to contain many more of the 
common species ; and a glance at the table wiU also prove that the shires bordering around 
Glasgow ha ve been more fully explored than almost any others, and if the other caj'boniferous 
fossils had been included in the list, it would ha%'e been likewise seen that the Glasgow dis- 
trict is by far the richest fossiliferous portion of Scotland. 
