DAVIDSON — SCOTTISH CARBONIFEEOUS BEACHIOPODA. 



259 



SCOTTISH COUNTIES IN WHICH THE FOLLOWING CARBONIFEROUS 

 BRACHIOPODA HAVE BEEN DISCOVERED * 



Lanarkshire. 



Renfrewshire. 



Ayrshire. 



Buteshire. 



Dumbartonshire. 



Stirhngshire. 



Dumfriesshire. 



Peebleshire. 



Edinburghshire. 



Linlithgowshire. 



Hadding-tonshire. 



Fifeshire. 



Berwickshire. 



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Geneha and Species. 



10. 

 11. 

 12. 

 13. 



14. 

 15. 

 16. 

 17. 

 18. 

 19. 

 20. 

 21. 

 22. 

 23. 



24. 



25. 

 26. 

 27. 

 28. 

 29. 

 30. 

 31. 



Terehratula hastata, Sow.. 



sacculus, Martin 



vesicularis, de Kon 



Spirifera dupUcicosta, Phil. 



hisulcata, Sowerby. 



trigonalis, Sowerby 



ovalis, Phillips 



ping ids, Sowerby. . , 



glabra, Martin 



Urii, Fleming .. .. 



CarluTciensis, Dav.. 



lineata, Martin 



Spiriferina cristata, var. oc 



toplicata, Sowerby 



insculpta, Phillips 



Imninosa, M'Coy 



Athyris amhigtia, Sowerby 



pilano- sulcata, Phil 



Royssi, rEveille 



Betzia raclialis, Phillips 

 Bhynchonella pugnus, Mar 



pleuTodon, Phil 



Camarophoria crmnena, Sow 

 Strophomena rhom^oidaUs 

 var. analoga and distorta 



Sowerby 



Streptorliynchus crenistria. 

 Phillips, and var. radialis 



and var. Kellii 



OrtJiis resiipinata, Martin, 



MiclieUni, I'EveiUe . . . 



Chonetes Hardrensis, Phil. . 



Buchiana, de Kon. . 



Productus giganteus, Martin 



latissirmis, J. Sow 



cor a, d'Orbigny... 



* This Table shows the Shires in which Carboniferous strata exist, as well as the amount of 

 work done in the way of collecting organic remains. Those counties from which few species 

 are recorded will no doubt upon fuller exploration be found to contain many more of the 

 common species ; and a glance at the table will also prove that the shires bordering around 

 Glasgow have been more fully explored than almost any others, and if the other cai-boniferous 

 fossUs had been included in the hst, it would have been Ukev/ise seen that the Glasgow dis- 

 trict is by far the richest fossiUferous portion of Scotland. 



