OLAF HuI.TKDAHL. [SEC. ARCT. EXP. FRAM 



I'liim/i.- i Srlteii imv. num. 



7'//(///>.va.s7/-.i V' i-iinn'i M. Ki'-.v \- HAI.MF. 



..]/ siiliorliirnlii i 'IK I.\M 



iini"l'iirn Meii'-i'i \.t.\\ ^ 



I I'lhi/niii'lld tnuttistriata ll\ii. 

 />lii'iniiD/t,i varistriata (.UNRAD. 



l-i-"'lii<-lfll,i itri'tii-iixtrntd HALL. 



r,-u,l,-li'll<t xnb<tcnlfitfii Mi KIM. var. l<itir di'iticn. 

 .Itrif/in 1-i-Hcttlnri* I.INM 

 ~ />n l/i'l- Srl/'-ii MINI li. 

 N/// ;//(/ fli'i/nn* >IMN var. 

 y. ////.-, ' /MS I '.I \rr. 



SclI.NL'K. 



i-incei>s BAKU. 



Sow ? 

 I fit 



SCIIM;R. 



A> to the age and relatiuiiri of these faunas, the following staleinents 

 art- made by the two paleontologists: 



Db belongs to Lower Heidelberg, probably to the middle of that 

 division. 



Do must be of a distinctly younger age than Db. though no distinct 

 hori/on can be lixrd. 



Dtl, De, Df point towards Uppermost Lower Devonian, and 

 lower M id (I le Dev o n ian. 



Dg is of Middle Devonian age. 



Dh is. according to LOEWE, to be placed about the boundary of the 

 Middl.'-l'ppcr Devonian. According lo MKYKK Dh as well as Di is of 

 C|i|"'i' Devonian age and point toward Chemung. 



I'rof. .1. Ki.rii in his |aper: Upper Devonian Fish remains from Klle>- 

 inere Land" (this report no. 33. l!Hf>| has from Dh de>ci ibed a cranial shield 

 of a fish Macropetdlichthys Solicit KI.KH. and concludes as lo the age of the 

 -aid /.one that it >hould most probably be aligned lo the Ira us it ion 

 -I rat a between the Middle and Upper Devonian. It does not 

 -mi likely that -o young a hori/on as ( Ihemung is represented in series 

 D at all. 



With transitional /.one- carrying sandstone bed- the marine Series 

 1 1 passes into Sene- I-!, consisting of at least 11 -TOO m. of sandstone, 

 \v|i () ~ ( . .--nilial fo--il> are .-cant\ li-h and plant remains. The loriner 

 ha\. bei-n de-cribed by Ki.i:i{ in the paper just mentioned. From the 

 middle part ,,f the -cries are identified the following fossils: 



