New Britain Trench

Short description: Oceanic trench in the southern Pacific Ocean

New Britain

Papua
New
Guinea

Woodlark
Island

Solomon
Islands

Louisiade Archipelago

Coral
Sea
Basin

Woodlark Basin

Manus
Basin

Louisiade
Plateau

Ontong
Java
Plateau

Britain
New Trench

Woodlark Rise

Papuan
Plateau

Trobriand
Trough

Pock-
lington
Trough

Solomon
Sea

Pocklinton Rise

Seafloor topographic map of area adjactent to New Britain Trench.

<mapframe zoom="5" text="Approximate surface projection on Pacific Ocean of New Britain Trench (blue)." align="right" height="250" latitude="-7" longitude="153" width="330">{{Wikipedia:Map data/New Britain subduction zone}}</mapframe> The New Britain Trench (also known as Bougainville-New Britain Trench or New Britain-Solomon Trench)[1] has formed due to subduction of the floor of the Solomon Sea and has some of the highest current seismic activity in the world.[2]

The trench was discovered by the German research vessel SMS Planet, in 1910.[3]

## Contents

* 1 Geography
* 1.1 Tectonics
* 1.2 Associated seismicity
* 1.3 Associated volcanism
* 2 Ecology
* 3 References

## Geography

The trench is 840 km (520 mi) long,[2] curved around the south of New Britain and west of Bougainville Island in the northern Solomon Sea. The deepest point is the Planet Deep at 9,140 m (29,990 ft).[2]

### Tectonics

The New Britain subduction zone is a continuum with the Vanuatu subduction zone and are all cases of subduction polarity reversal as originally the Pacific Plate subducted under the Indo-Australian Plate's minor plates such as the North Bismarck Plate. However now minor plate subduction is associated with the Australian Plate subducting under the Pacific Plate. In this case it is the Solomon Sea Plate and Trobriand Plate subducting under the South Bismarck Plate.[4] It is possible that the collision to the west of the 30–35 km (19–22 mi) thick Ontong Java Plateau with the Vitiaz Trench from about 25 million years ago initiated this polarity reversal.[5] The rates of subduction and roll back are high and are currently for the New Britain Trench, a subduction velocity of 65–120 cm/year (26–47 in/year), a convergence velocity of 2–48 cm/year (0.79–18.90 in/year), and spreading deformation rate in its arc-back- arc area of 10–74 cm/year (3.9–29.1 in/year).[6] In various parts of the trench there is up to 18 cm/year (7.1 in/year) of trench roll back and 20 cm/year (7.9 in/year) of trench advance.[6]

### Associated seismicity

The New Britain subduction zone is extremely seismically active and has had more than 22 earthquakes with magnitudes equal to or larger than 7.5 since 1990.[7]

### Associated volcanism

There is quite active arc volcanism with for example the active Rabaul Caldera area in the north east of New Britain having had a recent series of euptions in 1994 that destroyed the port of Rabaul.[8]

## Ecology

The diversity of life forms discovered living on top of the trench floor sediments and scavenging communities is high, [9] with during one study at 1 km (0.62 mi) depth 35 species observed, with biodiversity decreasing at 3.7 km (2.3 mi) depth before increasing again at 8.2 km (5.1 mi).[10] This is likely to reflect several factors. The trench is situated within the southern West Pacific Warm Pool characterized by sea surface temperature greater than 28°C and because of its closeness to tropical land, the land is subject to high rain fall.[11] The trench is only 55 km (34 mi) offshore from New Britain with an almost uniform slope into it of about 8°.[7] Hence there is a very high organic carbon load, sourced more than other trenches from soil organic matter, although marine phytoplankton and a minor contribution from land plants also help.[12]

Species observed at 1 km (0.62 mi) depth included a free swimming Teuthidodrilus (squidworm).[10] and ulmarid jellyfish.

At 8.7 km (5.4 mi) depth starfish and shrimps believed to be either of the family Penaeidae or the order Mysida were observed.[10] There were 5 amphipod species including Alicella gigantea.[13] Novel viruses and bacteria have been characterised in the sediment collected at this depth.[14][15]

## References

1. ↑ Marine Gazetteer:New Britain Trench
2. ↑ 2.0 2.1 2.2 Gallo et al. 2015, p. 120.
3. ↑ GEBCO:New Britain Trench
4. ↑ Benyshek & Taylor 2021, 6.3.1.Case 2: Four-Plate Solution, Figure 11.
5. ↑ Li et al. 2023, Section: 2.1 Polarity-reversal subduction initiation.
6. ↑ 6.0 6.1 Li et al. 2023, Table 2, p482.
7. ↑ 7.0 7.1 Luo et al. 2019, p. 1682.
8. ↑ McKee & Duncan 2016.
9. ↑ Gallo et al. 2015, p. 119.
10. ↑ 10.0 10.1 10.2 Gallo et al. 2015, pp. 126-127.
11. ↑ Luo et al. 2019, p. 1681.
12. ↑ Luo et al. 2019, p. 1680.
13. ↑ Gallo et al. 2015, p. 128.
14. ↑ Hui, Zhou; Ping, Chen; Mengjie, Zhang; Jiawang, Chen; Jiasong, Fang; Xuan, Li (2021). "Revealing the Viral Community in the Hadal Sediment of the New Britain Trench". Genes 12 (990): 990. doi:10.3390/genes12070990. PMID 34209474.
15. ↑ Wei, Y; Fang, J; Xu, Y; Zhao, W; Cao, J (2018). "Corynebacterium hadale sp. nov. isolated from hadopelagic water of the New Britain Trench". International Journal of Systematic and Evolutionary Microbiology 68 (5): 1474–8. doi:10.1099/ijsem.0.002695. PMID 29557772.

Sources

* Li, M; Huang, S; Hao, T; Dong, M; Xu, Y; Zhang, J; He, Q; Fang, G (2023). "Neogene subduction initiation models in the western Pacific and analysis of subduction zone parameters". Science China Earth Sciences 66 (3): 472–91. doi:10.1007/s11430-022-1065-1.
* Benyshek, E. K.; Taylor, B. (2021). "Tectonics of the Papua-Woodlark region". Geochemistry, Geophysics, Geosystems 22 (e2020GC009209). doi:10.1029/2020GC009209.
* Gallo, ND; Cameron, J; Hardy, K; Fryer, P; Bartlett, DH; Levin, LA (1 May 2015). "Submersible-and lander-observed community patterns in the Mariana and New Britain trenches: influence of productivity and depth on epibenthic and scavenging communities". Deep Sea Research Part I: Oceanographic Research Papers 99: 119–33. doi:10.1016/j.dsr.2014.12.012.
* Luo, M; Gieskes, J; Chen, L; Scholten, J; Pan, B; Lin, G; Chen, D (2019). "Sources, degradation, and transport of organic matter in the New Britain Shelf‐Trench continuum, Papua New Guinea". Journal of Geophysical Research: Biogeosciences 124 (6): 1680–95. doi:10.1029/2018JG004691.
* McKee, CO; Duncan, RA (2016). "Early volcanic history of the Rabaul area". Bulletin of Volcanology 78 (4): 1–28. doi:10.1007/s00445-016-1018-3.

[ ⚑ ]  6°00′S 152°30′E﻿ / ﻿6°S 152.5°E﻿ / -6; 152.5

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