RARITAN FORMATION— CORRELATION. 23 



Ilex aniboyensis Berry. 



LaurophyUiim lanceolatiim Newb. 



Laurophyllmn mimts Newb. 



Leguminosites raritanefiis Berry. 



Liriodendron qiiercifolium Newb. 



Menispermitcs Wavdianns Hollick. 



Myrica acuta Hollick. 



Myrica cinnamomifolia Newb. 



Myrica fenestrata Newb. 



Myrica Hollicki Ward. 



Myrica Nezvherryana Hollick. 



Myrica raritanensis Hollick. 



Myrsine oblongata Hollick. 



Newherryana rigida (Newb.) Berry. 



Passiflora antiqua Newberry. 



Planera Knowltoniana Hollick. 



Persoiiia spatulata Hollick. 



PhylUtes trapoformis Berry. 



Phyllitcs undulatiis Newb. 



Podo2aniitcs aciiminatiis Hollick. 



Populus orbicularis (Newb.) Berry. 



Protophyllum obovatuui Newb. 



Primus ? acutifolia Newb. 



Qiicrciis raritanensis Berry. 



Rhamniies minor Hollick. 



Salix pseiido-H\ayei Berry. 



Sphaerites raritanensis Berry. 



Williamsonia Smockii New^b. 

 Obviously these are of little service in correlation, neverthe- 

 less all but one or two are dicotyledons of genera, which in 

 Europe are found only in the Cenomanian and Senonian. Allied 

 forms are largely represented in the Magothy formation, the 

 Dakota Group, and the Atane beds of Greenland. 



There are 10 Lower Cretaceous species which persist into 

 the Raritan. These are : 



Aspleninni Dicksoniamun Heer. 



Celastrophyllnni Brittonianum Hollick. 



Frenelopsis Hoheneggeri (Ettings.) Schenk. 



