CHAMBERLIN: THE CHILOPODA OF BRAZIL. 157 
CRYPTOPS IHERINGI Brélemann. 
Rev. Museu Paulista, 1901, 5, p. 42, pl. 1, fig. 6, 7; Kraepelin Revis. Scolop., 
1903, p. 32, fig. 2; Brélemann, Cat. Myr. Brésil, 1909, p. 8. 
Localities.— State of Sdo Paulo: Alto da Serra (type loc.); State of 
Rio de Janeiro: Petropolis; State of Rio Grande do Sul. 
CRYPTOPS GALATHEAE Meinert. 
Vidensk medd. nat. foren. Kj@benhavn, 1887, p. 140; Kraepelin, Revis. Scolop., 
1903, p. 54. 
Cryptops capivarae Pocock, Ann. mag. nat. hist., 1891, ser. 6, 8, p. 158; Bréle- 
mann, Cat. Myr. Brésil, 1909, p. 8. 
Cryptops brasiliensis Attems, Mitt. Mus. Hamburg, 1900, 18, p. 112; Brdle- 
mann, Cat. Myr. Brésil, 1909, p. 8. 
Localities — State of Rio Grande do Sul (braszliensis Attems); State 
of Matto Grosso: Rio Capivari (capivarae Pocock); Argentina: 
Montevideo (galatheae Meinert). 
CRYPTOPS HEATHI, sp. nov. 
Color yellowish. Head a little darker than the body. 
Head widest anteriorly, the sides converging caudad; caudal mar- 
gin straight, meeting the edge of the first dorsal plate flush or scarcely 
overlapping the latter. Sulci not evident in middle and anterior 
portions; but rather faintly indicated caudad. Scarcely punctate. 
Prosternum not punctate; with a median longitudinal furrow. 
Anterior margin nearly straight, being very ‘slightly bowed caudad 
toward each end; bearing three bristles on eaeh side. (Plate 1, fig. 2). 
First dorsal plate with a distinct transverse cervical sulcus which 
is angularly bent caudad at the middle line, the plate being depressed 
at this angle. Two longitudinal sulci present, but these in the type 
are rather weak; forking cephalad, the inner branches meeting at an 
angle at the median line a little caudad of the cervical sulcus and the 
lateral lines each meeting the sulcus farther laterad (see Plate 1, fig. 1). 
All dorsal plates from the second to twentieth longitudinally bisul- 
cate. Plates not roughened; none of them bearing cornicles. 
Last plate with a shallow median longitudinal furrow which is more 
evident toward the caudal end. 
