Overlaps in the region with Late-Lapita. In New Ireland, undecorated globular jars and restricted necks and out curving rims, with incision and some applied relief (bands and nubbins), lip-notching and red slip. In Tanga and New Ireland, the placer and sand tempers become more frequent (than calcareous) in transitional, although though they are present in Middle/Late Lapita and the calcareous are still present in Transitional.
Admiralty Transitional (2300 - 1900 BP)
Admiralty Islands Wikidata ID: Q119230
Manus Province Wikidata ID: Q874935
| None (0) | Minor (1) | Few (2) | Common (3) | Frequent (4) | Major (5) | Very Dominant (6) |
| 0% | 0-5% | 5-15% | 15-30 % | 30-50% | 50-70% | 70-100% |
| Name | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics/ Region |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr101 | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland feldspathic non-placer | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr102 | 0 | 0 | 3 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland pyroxene rich-placer | 0 | 0 | 3 | 3 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr102a | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland placer | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr103 | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| New Ireland volcanic sand | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr104 | 1 | 0 | 1 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| New Ireland pyroxenic placer | 0 | 0 | 1 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr105 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| New Ireland calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr106 | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Exotic New Ireland quartz-calcite | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr107 | 0 | 0 | 6 | 4 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| New Ireland feldspathic-pyroxenic | 0 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr108 | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| New Ireland placer beach | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr134 | 1 | 0 | 2 | 5 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| TLTF olivine placer | 0 | 0 | 0 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr178 | 0 | 1 | 4 | 3 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| Bismarck pyroxenic | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Bismarck |
| tpr179 | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, lathwork |
| Bismarck feldspathic | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Bismarck |
| tpr180 | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Bismarck lithic | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Bismarck |
| tpr313 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Tanga calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr315 | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Tanga feldspathic pyroxenic mica | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr316 | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Tanga feldspathic pyroxenic | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr317 | 0 | 0 | 2 | 6 | 0 | 3 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| Tanga pyroxene placer | 0 | 0 | 1 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr318 | 2 | 0 | 2 | 5 | 1 | 6 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic |
| Tanga pyroxene opaque placer | 0 | 0 | 1 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr319 | 0 | 0 | 1 | 2 | 0 | 6 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| Tanga opaque placer | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr320 | 3 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, felsitic, vitric |
| Tanga lithic hybrid | 2 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Bismarck |
| tpr321 | 0 | 0 | 3 | 2 | 2 | 6 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| Exotic Tanga hornblendic hybrid | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Bismarck |
| tpr322 | 0 | 0 | 6 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| Tanga hornblendic pyroxenic | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr191a | 1 | 0 | 2 | 4 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| Manus andesitic placer | 0 | 0 | 2 | 4 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr92 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Mussau type A | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| Slide | Fabric | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_31_1 | tpr101 (New Ireland feldspathic non-placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_31_3 | tpr102 (New Ireland pyroxene rich-placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 4 | 4 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_31_10 | tpr102a (New Ireland placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_41_16 | tpr105 (New Ireland calcareous) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_31_23 | tpr107 (New Ireland feldspathic-pyroxenic) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_41_19 | tpr107 (New Ireland feldspathic-pyroxenic) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 4 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_41_21 | tpr107 (New Ireland feldspathic-pyroxenic) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 4 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_31_24 | tpr108 (New Ireland placer beach) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_102_1 | tpr134 (TLTF olivine placer) | TLTF or New Britain | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 2 | 5 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_102_2 | tpr178 (Bismarck pyroxenic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 1 | 3 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_102_4 | tpr178 (Bismarck pyroxenic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 4 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_102_3 | tpr179 (Bismarck feldspathic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, lathwork |
| WD_102_5 | tpr180 (Bismarck lithic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| WD_33_1 | tpr313 (Tanga calcareous) | Tanga | Transitional Far Western (2350 - 1900 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_33_13 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_33_11 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_33_5 | tpr316 (Tanga feldspathic pyroxenic) | Tanga | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_30_8 | tpr318 (Tanga pyroxene opaque placer) | Tanga | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 1 | 3 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| WD_30_2 | tpr317 (Tanga pyroxene placer) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 1 | 6 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| WD_41_4 | tpr191 (Manus andesitic) | Manus | Admiralty Transitional (2300 - 1900 BP) | 0 | 0 | 4 | 3 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
Feldspathic non-placer sand temper.
Pyroxene-rich beach placer sand temper.
Hornblende-rich, feldspathic sand temper of probable beach origin.
Calcareous sand temper, rare plagioclase and clinopyroxene.
Moderately sorted and subrounded sand temper of probable stream origin that is plagioclase-rich.
Volcanic sand temper.
Feldspathic sand temper.
Well sorted placer sand temper of probable beach origin that contains subordinate but prominent hornblende grains. Leached calcareous.
Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands Olivine and hornblende present. Has orthopyroxene in addition to the more abundant clinopyroxene. Microlitics are hyalopilitic.
Non-Lapita. Moderately sorted, subangular to subrounded aggregates, probably stream sands. Microlitic volcanic rock fragments are hyalopilitic.
Non-Lapita. Moderately sorted, subangular to subrounded aggregates, probably stream sands. Microlitic lithics are hyalopilitic.
Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands. Volcanic rocks are felsitic (microcrystalline quartz-feldspar groundmass mosaic commonly with plagioclase microphenocrysts).
Non-Lapita. Vitric glass. Well sorted, subrounded to subangular aggreates that are probably beach sands. Microlitic lithics are hyalopilitic.
Exclusively calcareous temper sand. From reef. From Lifafaesing.
Lifafaesing site. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Angkikita site. Feldspathic temper sand that contains abundant clinopyroxene and biotite.
Angkikita site. Feldspathic temper sand that contains abundant clinopyroxene and no biotite.
Angkikita. Mixed pyroxene/opaque iron oxide ferromagnesian placer sand temper.
Lifafaesing. Pyroxene-rich ferromagnesian placer sand temper.
Quartz-free andesitic temper sand. Stream sand present. Pyroxene < Hornblende.