| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | II.—On the Punctation of the Shells of Terebratula |
|---|
| Journal | Geological Magazine |
|---|
| Year | 1916 (February) | Series:Volume | 6:3 |
|---|
| Issue | 2 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800191125 |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 264231 | Long-form Identifier | mindat:1:5:264231:8 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | (1916) II.—On the Punctation of the Shells of Terebratula. Geological Magazine, S. 6 Vol. 3 (2) 51-56 doi:10.1017/s0016756800191125 |
|---|
| Plain Text | (1916) II.—On the Punctation of the Shells of Terebratula. Geological Magazine, S. 6 Vol. 3 (2) 51-56 doi:10.1017/s0016756800191125 |
|---|
| In | (1916, February) Geological Magazine S. 6 Vol. 3 (2) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | In 1844 Carpenter [1] divided the fossils then known as Terebratula into two groups—a perforate group, having the test covered with minute pores, and an imperforate group (the Rhynchonellids). These perforations (see Plate III) correspond to tubular processes of the mantle. |
|---|
These are possibly similar items as determined by title/reference text matching only.
