278 Notices of Memoirs — Dr. G. Linnarsson — Graj^tolite Schists. 



19. Cypris ? fasciculata, E. F. 



20. ? grannlata, E. F. (? C. granulosa, Dunker.) 



c. — Lower Puebeck. 



21. Cypris ? Purbeckensis, E. F. 



22. ^punctata, E. F. 



These are figured in Sir C. Lyell's " Manual of Geology," see Geol. Mag. I.e. p. 105. 



Note on the Distribution of the Species. 

 Nos. 1, 11, and 13. Very common throughout the Wealden and in some Purbeck beds ; also in 

 Germany. 



2 and 12. Rather rare. Figured by Fitton from some unmentioned locality ; Peasemarsh, 



Surrey ; ShotoTer. 



3 and 16. Not uncommon in the Wealden Beds. In the Upper Purbeck. 



4. Accompanies 0. tuherculata in some places. 



5. Hastings beds of Sussex ; Purbeck beds of South Wilts. 



6. Not uncommon in the Wealden beds. 



7. Shotover; Obernkirchn, Hanover. 

 8 and 9. Shotover. 



10. Shotover. 

 14 and 20 ? Sub wealden Boring, Sussex ; Hanover; Middle Purbeck of Dorset? 



Addenda et Corrigenda. — At page 101, line 25, add : It occurs 

 throughout a bed about 15 feet thick, and is very characteristic of 

 the zone. At p. 101, add: Estheria tenella (Jordan), "Monogr. Foss. 

 Estheriae," 1862, p. 31, etc., has been found abundantly by the 

 Geological Surveyors of Scotland in the Coal-measures near Airdrie ; 

 and, in one instance (at Glenmavis Burn), it constitutes a bituminous 

 shale, so thickly are the individuals massed together. From Palace- 

 craig, near Airdrie, where E. tenella has lately been obtained, I 

 remember to have seen specimens of a much larger Estheria, since 

 lost. At p. 102, line 16 from bottom, for Fred, read Ferd. At 

 p. 105, line 23, for on read in. Line 32, after figured specimen, 

 add: = Cypridea Austeni. At p. 109, line 8 from bottom, add: 

 Mr. H. Caudell has also found Cypridea Valdensis in the Ironstone 

 of Wheatley, two miles S.E. of the other locality. 



iTOTiOES OIF nvnEHVnoiies. 



I. — On the Geaptolite Schists of Kongslena in "Westrogothia, 

 Sweden.^ By Dr. G. Linnarsson, Director of the Geological 

 Survey of Sweden. 



IN the Upper Graptolite schists of Westrogothia two divisions are 

 recognizable — a lower division characterized by Monogr. lohiferus 

 (M'Coy) and Bastrites peregrinus (Barr.) ; and a higher division 

 characterized by Monograpt. priodon (Bronn) and Betiolites Geinitz- 

 ianus (Barr.). The same divisions, well separated, appear in other 

 parts of the country, and Tornquist has already proposed for them 

 the respective titles of the Lohiferus Schists and Betiolites Schists.^ 



Among the localities in Westrogothia vi'here the Upper Graptolite 

 Schist is most accessible is Strommen in the parish of Kongslena. 

 These schists, as well as the immediately underlying strata, the 

 Brachiopod Schists and the Trinucleus Schists, are locally cut into 

 by a considerable stream. The Lohiferus Schist is here a black 



' Abstract of a paper published in the Geologiska Foreningens i Stockholm For- 

 handlingar, 1877, Nr. 41 ; Bd. III., Nr. 13. 



2 Tornquist, Ofvers. af K. Vet. Akad. Forhandl., 1875, p. 57. 



