Neoselachians from the Danian (early Paleocene) of Denmark

TY - JOUR

T1 - Neoselachians from the Danian (early Paleocene) of Denmark

AU - Adolfssen, Jan Schulz

AU - Ward, David J.

PY - 2015

Y1 - 2015

N2 - A diverse elasmobranch fauna was collected from the early Danian Rødvig Formation and the early to middle Danian Stevns Klint Formation at Stevns Klint and from the middle Danian Faxe Formation at Faxe, Denmark. Teeth from 27 species of sharks are described including the earliest records of Chlamydoselachus and Heptranchias howelli from Europe. The fauna collected at the Faxe quarry is rich in large species of shark including Sphenodus lundgreni and Cretalamna appendiculata and includes no fewer than four species of Hexanchiformes. The species collected yield an interesting insight into shark diversity in the Boreal Sea during the earliest Paleogene. The early Danian fauna recorded from the Cerithium Limestone represents an impoverished Maastrichtian fauna, whereas the fauna found in the slightly younger bryozoan limestone is representative of a pronounced cold water fauna. Several species that hitherto have only been known from the Late Cretaceous have been identified, clearly indicating that the K-T boundary was not the end of the Cretaceous fauna; it lingered and survived into the early Danian.

AB - A diverse elasmobranch fauna was collected from the early Danian Rødvig Formation and the early to middle Danian Stevns Klint Formation at Stevns Klint and from the middle Danian Faxe Formation at Faxe, Denmark. Teeth from 27 species of sharks are described including the earliest records of Chlamydoselachus and Heptranchias howelli from Europe. The fauna collected at the Faxe quarry is rich in large species of shark including Sphenodus lundgreni and Cretalamna appendiculata and includes no fewer than four species of Hexanchiformes. The species collected yield an interesting insight into shark diversity in the Boreal Sea during the earliest Paleogene. The early Danian fauna recorded from the Cerithium Limestone represents an impoverished Maastrichtian fauna, whereas the fauna found in the slightly younger bryozoan limestone is representative of a pronounced cold water fauna. Several species that hitherto have only been known from the Late Cretaceous have been identified, clearly indicating that the K-T boundary was not the end of the Cretaceous fauna; it lingered and survived into the early Danian.

KW - Cerithium Limestone

KW - Chondrichthyes

KW - Danian

KW - Denmark

KW - Faxe Formation

KW - Paleocene

U2 - 10.4202/app.2012.0123

DO - 10.4202/app.2012.0123

M3 - Journal article

AN - SCOPUS:84930841037

SN - 0567-7920

VL - 60

SP - 313

EP - 338

JO - Acta Palaeontologica Polonica

JF - Acta Palaeontologica Polonica

IS - 2

ER -