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 |
| |
H. euphratis - broad disjunct bar | NN1-3 |
| |
H. intermedia - narrow disjunct bar |
NN1-11 |
| |
H. granulata - granular central area, without real pores |
NN1-10 |
| |
H. carteri - pores inline |
NN1-21 |
| |
H. wallichii - pores oblique |
NN11(?)-21 |
| |
H. sellii - pores large |
NN12-19 |
| |
H. inversa - pores separated by inversely oriented bar (points toward flange termination) | NN19-20 |
| H. pavimentum - small, narrow flange, inline pores | NN19-21 |