H. carteri group

Citation: 
H. carteri group of Young (1998)

These are medium to large species (typically 7-11 microns) with flanges that end in distinct wings. They are the most common helicoliths in most samples, but vary markedly through the Neogene. Forms with disjunct (optically discontinuous) bars (H. euphratis & H. intermedia) dominate in the Early Miocene but are replaced progressively by forms with closed central areas or conjunct bars. The blankets on these are initially rather chaotic (H. granulata) but forms with well ordered blankets with two in-line pores (H. carteri) become more common through the Late Miocene. In the Pliocene, forms with large and/or oblique pores (H. sellii and H. wallichii) become common.

Drawing Outline description Range
euphratis_Theod84.jpg H. euphratis - broad disjunct bar NN1-3
intermedia_Theod84.jpg H. intermedia - narrow disjunct bar
NN1-11
sketch Hgranul H. granulata - granular central area, without real pores
NN1-10
paleocarteri_Theod84.jpg H. carteri - pores inline
NN1-21
wallichii_Theod84.jpg H. wallichii - pores oblique
NN11(?)-21
sketch Hsell H. sellii - pores large
NN12-19
inversa_Theod84.jpg H. inversa - pores separated by inversely oriented bar (points toward flange termination) NN19-20
sketch Hpavim H. pavimentum - small, narrow flange, inline pores NN19-21
Scratchpads developed and conceived by: Vince Smith, Simon Rycroft & Dave Roberts