Articoli di riviste: "Gulf of Papua"

1

Wolanski, Eric, Alain Norro e Brian King. "Water circulation in the Gulf of Papua". Continental Shelf Research 15, n. 2-3 (febbraio 1995): 185–212. http://dx.doi.org/10.1016/0278-4343(94)e0026-i.

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2

GASSMANN, DIRK, e STEPHEN J. RICHARDS. "Two new damselflies of the genus Idiocnemis Selys from Gulf Province, Papua New Guinea (Odonata: Platycnemididae)". Zootaxa 4560, n. 1 (22 febbraio 2019): 121. http://dx.doi.org/10.11646/zootaxa.4560.1.6.

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Two new species of the genus Idiocnemis Selys, 1886 from southern Papua New Guinea are described: Idiocnemis lakekamuensis sp. nov. from the Lakekamu Basin and I. milou sp. nov. from Lakekamu and the Kikori River lowlands. Males and females are illustrated and compared with other species of the Idiocnemis bidentata group. Both new species are known only from the Papuan Gulf Foreland area of endemism and may be considered endemic to it.

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3

Harrington, Amanda, Cyrille Reiser, Bob Burmaz e Rod Reed. "Amplitude-versus-offset (AVO) screening in frontier basins: an example from the Gulf of Papua, Papua New Guinea". APPEA Journal 52, n. 2 (2012): 701. http://dx.doi.org/10.1071/aj11115.

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A resurgent interest in the gas potential of the Gulf of Papua has been enhanced by the recent announcement of developing new LNG facilities in Port Moresby. Petroleum Geo-Services (PGS) has recently acquired a 6,000-km2 Multi-Client 3D (MC3D) survey in the gulf. Although most of the discoveries in PNG are from the highland areas, the gulf is a proven hydrocarbon province with gas/condensate accumulations previously discovered in several reef build-ups. It is thought that sediments from the Papuan Fold Belt produced clastic dominated deltas in the Gulf area. Although this play is untested offshore, there is evidence these sandy facies exist and could contain hydrocarbons. On the first phase of acquisition/interpretation, an efficient screening workflow called Prospect Scanner, developed to highlight areas of AVO effects in large 3D seismic datasets, was tested. It uses pre-stack seismic time migrated (PSTM) gathers to extract AVO attributes that are then inverted to derive relative acoustic and shear impedance volumes. Using idealised cross-plots, the relationship between Vp/Vs ratio and the Ip values gives a good indication of the fluid and lithology of the tested interval. The results are loaded into a conventional interpretation package for interpretation/visualisation. Prospect Scanner has highlighted previously undrilled turbidite and basin floor fan prospects in the region. The Vp/Vs versus Ip cross-plot shows clustering of the sand anomaly and good separation from the majority of the plot. These points correspond to the idealised location for a gas sand. Past concerns about lateral prediction of reservoir presence and quality associated with the basin floor fans can be addressed through this workflow.

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4

Amiribesheli, Said, e Andrew Weller. "The prospectivity of the Cape Vogel Basin, Papua New Guinea". APPEA Journal 59, n. 2 (2019): 840. http://dx.doi.org/10.1071/aj18094.

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The frontier and underexplored Cape Vogel Basin (CVB), north of the Papuan Peninsula, is thought to be underlain by Late Palaeocene–Eocene oceanic crust and overlain by Cenozoic sediments. Several impartial data provide evidence of working petroleum system(s) including a flow of oil from a 1920s well, and two 1970s wells that encountered minor hydrocarbon traces and good source material. The 1970s wells chased Miocene reef plays (like the discoveries in the Gulf of Papua). No Miocene reefs were encountered, with both wells terminating in volcanics. Integration of open-file 2D seismic, modern 2D PSDM seismic and shipborne gravity and magnetic data improves the subsurface imaging and thus understanding of prospectivity. The data reveal a significant sedimentary section (including Mesozoic sediments) and that the volcanics are not laterally continuous (i.e. products of short periods of volcanism). The data also suggests several Mesozoic–Cenozoic plays (e.g. carbonate reefs, incised canyons). Repeatable sea surface slicks, and observable bottom-simulating reflectors and direct hydrocarbon indicators, also provide evidence of working petroleum system(s). It is hypothesised that the CVB has affinities with the Gulf of Papua with the extension of the Australian craton north of the Papuan Peninsula, with widespread deposition in the Mesozoic–Cenozoic, and with source rocks estimated to be within the hydrocarbon generative window. With incorporation of onshore data and presence of significant gravity low, it is postulated that the central and north-west were less susceptible to Late Cretaceous and Palaeocene differential uplift and erosion (related to Coral Sea breakup and extension), and thus have a higher chance of Late Mesozoic preservation.

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5

MacFarlane, JW, e R. Moore. "Reproduction of the ornate rock lobster, Panulirus ornatus (Fabricius), in Papua New Guinea". Marine and Freshwater Research 37, n. 1 (1986): 55. http://dx.doi.org/10.1071/mf9860055.

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Based on the examination of 26 499 female and 17 666 male specimens, the reproductive biology of P. ornatus is discussed with spatiotemporal reference to the annual breeding migration from northern Torres Strait to the Gulf of Papua. Migration commences generally in August with ovary development, mating and initial oviposition occurring during migration. Larval release normally commences once the migration has terminated on the reefs of the eastern seaboard in the Gulf of Papua. At the conclusion of the migration, marked segregation of the sexes occurs, with males entering shallow water (< 3 m) before females, who frequent deeper water (3-15 m) until their eggs have hatched. During the breeding season (November- April), females produce up to three broods. Fecundity is determined for 33 females in the carapace size range 75.4-121.0 mm. No significant egg loss during incubation was detected, but there was an indication of a reduction in the size of each subsequent brood. There appears to be a high post-spawning mortality of migratory lobsters. It is likely that the Gulf of Papua is the major source of larval recruitment in the western Coral Sea, including the east coast of Queensland and Torres Strait.

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6

Urwin, Chris. "Excavating and interpreting ancestral action: Stories from the subsurface of Orokolo Bay, Papua New Guinea". Journal of Social Archaeology 19, n. 3 (6 maggio 2019): 279–306. http://dx.doi.org/10.1177/1469605319845441.

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The Gulf of Papua, Papua New Guinea, is a rapidly changing geomorphic and cultural landscape in which the ancestral past is constantly being (re)interpreted and negotiated. This paper examines the importance of subsurface archaeological and geomorphological features for the various communities of Orokolo Bay in the Gulf of Papua as they maintain and re-construct cosmological and migration narratives. The everyday practices of digging and clearing for agriculture and house construction at antecedent village locations bring Orokolo Bay locals into regular engagement with buried pottery sherds (deposited during the ancestral hiri trade) and thin strata of ‘black sand’ (iron sand). Local interpretations and imaginings of the subsurface enable spatio-temporal interpretations of the ancestors' actions and the structure of ancestral settlements. These interpretations point to the profound entanglement of orality and material culture and suggest new directions in the comparative study of alternative archaeologies.

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7

Burns, K. A., P. Greenwood, R. Benner, D. Brinkman, G. Brunskill, S. Codi e I. Zagorskis. "Organic biomarkers for tracing carbon cycling in the Gulf of Papua (Papua New Guinea)". Continental Shelf Research 24, n. 19 (dicembre 2004): 2373–94. http://dx.doi.org/10.1016/j.csr.2004.07.014.

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8

Basiaco, Adriana, Chris Urwin e Tiina Manne. "Worked bone and teeth from Orokolo Bay in the Papuan Gulf (Papua New Guinea)". Australian Archaeology 86, n. 3 (27 agosto 2020): 226–37. http://dx.doi.org/10.1080/03122417.2020.1808560.

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9

Dharmawan, I. Wayan Eka, e Andriyani Widyastuti. "PRISTINE MANGROVE COMMUNITY IN WONDAMA GULF, WEST PAPUA, INDONESIA". Marine Research in Indonesia 42, n. 2 (19 settembre 2017): 73–82. http://dx.doi.org/10.14203/mri.v42i2.175.

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Papua shoreline has the most extensive area of mangrove in Indonesia. Since this area was rarely studied due to various reasons, the scientific data was difficult to be found. Wondama mangrove, part of Cendrawasih National Park – West Papua, had a promising mangrove forest to be discovered. Preliminary study was carried out in this area to identify how pristine the mangrove area is. The objectives of this study was to analyze mangrove community health and structure. Vegetation structure and canopy coverage data were collected from 107 circular plots included three plot areas (radian: 5 m, 2.5 m and 1 m) which were distributed to determine three plant classes i.e. tree, sapling and seedling, respectively. Present study showed that Wondama mangrove is a pristine mangrove community. It had large size of tree trunk diameter by 19.77± 6.55 cm averagely. Its diameter size affected on low tree density which was less than 1000 tree/ha. Those two parameters were strongly negative-correlated each other. On the other hand, community canopy was highly covered mangrove area by 82.46±6.43%. Rhizophora has mostly dominated in the forest. Mangrove regeneration in Wondama was excellent referring to density and species composition of sapling-seedling levels.

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10

Walsh, J. P., C. A. Nittrouer, C. M. Palinkas, A. S. Ogston, R. W. Sternberg e G. J. Brunskill. "Clinoform mechanics in the Gulf of Papua, New Guinea". Continental Shelf Research 24, n. 19 (dicembre 2004): 2487–510. http://dx.doi.org/10.1016/j.csr.2004.07.019.

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11

Zhiyu, Wang, e Carol A. Stein. "Subsidence of the Gulf of Papua in the Cenozoic". Tectonophysics 205, n. 4 (maggio 1992): 409–26. http://dx.doi.org/10.1016/0040-1951(92)90445-c.

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12

Nurulludin, Nurulludin, Suprapto Suprapto e Prihatiningsih Prihatiningsih. "PARAMETER POPULASI IKAN KAKAP LAUT-DALAM (Etelis radiosus, Anderson 1981) DI PERAIRAN TELUK CENDERAWASIH, PAPUA". BAWAL Widya Riset Perikanan Tangkap 8, n. 2 (13 gennaio 2017): 125. http://dx.doi.org/10.15578/bawal.8.2.2016.125-130.

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Ikan kakap laut-dalam (Etelis radiosus) adalah salah satu sumberdaya demersal ekonomis penting di Indonesia. Informasi ilmiah tentang ikan kakap laut-dalam ini masih sangat jarang, terutama dari kawasan Teluk Cenderawasih bagian Utara Papua. Penelitian ini dilaksanakan bulan Februari – November 2013 di Teluk Cenderawasih. Aanalisis panjang cagak ikan terhadap 3.255 ekor menggunakan software FISAT II, diperoleh beberapa nilai parameter populasi sebagai berikut: laju pertumbuhan (K) sebesar 0,17 per tahun, panjang asimtotik (L ) 108,68 cm FL, laju kematian alami (M) 0,4 pertahun, dan laju kematian karena penangkapan (F) 0,17 per tahun. Estimasi tingkat ekploitasi (E) sebesar 0,30 memiliki pengertian bahwa tingkat pemanfaatan ikan kakap laut dalam masih di rendah dan dapat ditingkatkan. Deep-sea snapper (Etelis radiosus) is one of high economic valued of demersal resources in Indonesia. Scientific information on deep-sea snapper is limited, especially from the northern part of Cenderawasih Gulf, Papua. This paper aims to determine some parameters populations of deepsea snapper (Etelis radiosus) in the gulf of Cenderawasih, Papua. The research conducted in February - November 2013 in the Gulf of Cenderawasih. Deepsea snapper fork length measurement randomly taken from 3.255 fishes in Nabire. The result obtained that the growth coefficient (K), asymptotic length (Linf)), natural mortality (M), fishing mortality (F) and exploitation rate (E) were 0.17/ year, 108.68 cmFL, 0.4/year, 0.17/year and 0.30/year. That implied the deepsea snapper fishing exploitation is under exploitation and there possibility of precountionary increasing of fishing effort.

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13

MICHALSKI, JOHN, STEPHEN RICHARDS e GUNTHER THEISCHINGER. "An interesting new species of Nososticta Hagen from southern New Guinea (Odonata, Disparoneuridae)". Zootaxa 3590, n. 1 (18 dicembre 2012): 73. http://dx.doi.org/10.11646/zootaxa.3590.1.7.

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Nososticta acuminata, a new disparoneurid damselfly from the Lakekamu Basin in Gulf Province of Papua New Guinea, is described. It is most similar to N. smilodon Theischinger & Richards, but the male has uniquely pointed superior anal appendages.

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14

Shearman, Philip L. "Recent Change in the Extent of Mangroves in the Northern Gulf of Papua, Papua New Guinea". AMBIO 39, n. 2 (marzo 2010): 181–89. http://dx.doi.org/10.1007/s13280-010-0025-4.

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15

Bird, M. I., A. R. Chivas e G. J. Brunskill. "Carbon-isotope composition of sediments from the Gulf of Papua". Geo-Marine Letters 15, n. 3-4 (settembre 1995): 153–59. http://dx.doi.org/10.1007/bf01204457.

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16

Webster, Jody M., Laura Wallace, Eli Silver, Bruce Applegate, Donald Potts, Juan Carlos Braga, Kristin Riker-Coleman e Christina Gallup. "Drowned carbonate platforms in the Huon Gulf, Papua New Guinea". Geochemistry, Geophysics, Geosystems 5, n. 11 (novembre 2004): n/a. http://dx.doi.org/10.1029/2004gc000726.

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17

Sembel, L., D. Setijawati, D. Yona e Y. Risjani. "Seasonal variations of water quality at Doreri Gulf, Manokwari, West Papua". IOP Conference Series: Earth and Environmental Science 890, n. 1 (1 ottobre 2021): 012007. http://dx.doi.org/10.1088/1755-1315/890/1/012007.

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Abstract The character of Manokwari City’s coastal waters is strongly influenced by activity on the mainland. The degradation in Sawaibu Gulf’s water quality has an impact on water quality nearby, as well as the waters of the Field Work Center (BLK), Lemon Island, and Tanjung Manggewa, which is part of Doreri Gulf. The purpose of this study was to determine the water quality in Doreri Gulf according on location and season. In February-April (rainy season) and August-October (dry season) 2020, the research was carried out within Doreri Gulf, Manokwari, West Papua. Turbidity, salinity, pH, temperature, and dissolved oxygen are amongst the variables analyzed. Its statistical analyses were performed descriptively using standard deviation and ANCOVA to correlate seasons and locations. Temperature, DO, and pH were highest at location 2; salinity showed highest at location 3; and turbidity were highest at location 1. Low concentrations of DO, pH, and salinity were measured at location 1; temperature showed highest at location 3; and turbidity were highest at location 1. The dry season would have the highest temperature, DO, pH, and salinity concentrations, meanwhile the rainy season had enough highest turbidity. The study confirms that there are no variations in water quality between location of each variable and that seasonal factors comprise the majority of differences in water quality.

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18

Bell, RS, PW Channells, JW MacFarlane, R. Moore e BF Phillips. "Movements and breeding of the ornate rock lobster, Panulirus ornatus, in Torres Strait and on the north-east coast of Queensland". Marine and Freshwater Research 38, n. 2 (1987): 197. http://dx.doi.org/10.1071/mf9870197.

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The principal biological question examined by the investigation was whether the resource of P. ornatus fished in Papua New Guinean waters was the same as that fished in Australian waters. In all, 11 932 specimens of Panulirus ornatus were tagged in Torres Strait and on the north-east coast of Queensland over a 3-year period from February 1980 to March 1983. By June 1984, 300 tagged P. ornatus had been recaptured. Of the 9632 P. ornatus tagged on the east coast of Queensland, none was recaptured in Torres Strait, while most of the 24 recaptures showing movements occurred to the south of the tagging sites. Of the 2300 P. ornatus tagged in Torres Strait, 8 were recaptured at sites to the north-east of the tagging sites in September and October 1980, coincident with the annual breeding emigration of P. ornatus from reefs in Papua New Guinean waters in northern Torres Strait, across the Gulf of Papua to breeding grounds near Yule Island. Results of this tagging study showed that P. ornatus from western Torres Strait also emigrate into Papuan New Guinean waters, where they are fished by both Australian and Papua New Guinean fishermen. However, recapture data also indicated that the population of P. ornatus in south-east Torres Strait and on the east coast of Queensland does not take part in this breeding emigration and may be a separate resource. During the study, 39 berried female P. ornatus were found on the north-east coast of Queensland but none in Torres Strait. The breeding stock near Yule Island may be the source of recruitment to both the Torres Strait and north-east coastal Queensland fisheries.

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19

Alongi, D. M., F. Tirendi e A. I. Robertson. "Vertical profiles of copper in sediments from the Fly delta and Gulf of Papua (Papua New Guinea)". Marine Pollution Bulletin 22, n. 5 (maggio 1991): 253–55. http://dx.doi.org/10.1016/0025-326x(91)90921-e.

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20

Apte, S. C., e G. M. Day. "Dissolved metal concentrations in the Torres strait and Gulf of Papua". Marine Pollution Bulletin 36, n. 4 (aprile 1998): 298–304. http://dx.doi.org/10.1016/s0025-326x(98)00188-x.

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21

Marcuson, Rachel, Jeffrey Gee, Emily Wei e Neal Driscoll. "A 2000 year geomagnetic field record from the Gulf of Papua". Marine Geology 408 (febbraio 2019): 48–66. http://dx.doi.org/10.1016/j.margeo.2018.11.014.

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22

Brunskill, Gregg J., Irena Zagorskis e John Pfitzner. "Geochemical mass balance for lithium, boron, and strontium in the Gulf of Papua, Papua New Guinea (project TROPICS)". Geochimica et Cosmochimica Acta 67, n. 18 (settembre 2003): 3365–83. http://dx.doi.org/10.1016/s0016-7037(02)01410-2.

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23

Alongi, D. M., S. G. Boyle, F. Tirendi e C. Payn. "Composition and Behaviour of Trace Metals in Post-oxic Sediments of the Gulf of Papua, Papua New Guinea". Estuarine, Coastal and Shelf Science 42, n. 2 (febbraio 1996): 197–211. http://dx.doi.org/10.1006/ecss.1996.0015.

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24

Bunch, Mark, Ric Daniel, Mark Lawrence, Greg Browne, Saju Menacherry, Tess Dance e Malcolm Arnot. "Multi-scale characterisation of the Paaratte Formation, Otway Basin, for CO2 injection and storage". APPEA Journal 52, n. 2 (2012): 664. http://dx.doi.org/10.1071/aj11078.

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A resurgent interest in the gas potential of the Gulf of Papua has been enhanced by the recent announcement of developing new LNG facilities in Port Moresby. Petroleum Geo-Services (PGS) has recently acquired a 6,000-km2Multi-Client 3D (MC3D) survey in the gulf. Although most of the discoveries in PNG are from the highland areas, the gulf is a proven hydrocarbon province with gas/condensate accumulations previously discovered in several reef build-ups. It is thought that sediments from the Papuan Fold Belt produced clastic dominated deltas in the Gulf area. Although this play is untested offshore, there is evidence these sandy facies exist and could contain hydrocarbons. On the first phase of acquisition/interpretation, an efficient screening workflow called Prospect Scanner, developed to highlight areas of AVO effects in large 3D seismic datasets, was tested. It uses pre-stack seismic time migrated (PSTM) gathers to extract AVO attributes that are then inverted to derive relative acoustic and shear impedance volumes. Using idealised cross-plots, the relationship between Vp/Vs ratio and the Ip values gives a good indication of the fluid and lithology of the tested interval. The results are loaded into a conventional interpretation package for interpretation/visualisation. Prospect Scanner has highlighted previously undrilled turbidite and basin floor fan prospects in the region. The Vp/Vs versus Ip cross-plot shows clustering ofthe sand anomaly and good separation from the majority of the plot. These points correspond to the idealised location for a gas sand. Past concerns about lateral prediction of reservoir presence and quality associated with the basin floor fans can be addressed through this workflow.

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25

Jablonski, D., S. Pono e O. A. Larsen. "PROSPECTIVITY OF THE DEEPWATER GULF OF PAPUA AND SURROUNDS IN PAPUA NEW GUINEA (PNG)—A NEW LOOK AT A FRONTIER REGION". APPEA Journal 46, n. 1 (2006): 179. http://dx.doi.org/10.1071/aj05011.

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Despite limited well control and paucity of seismic data, a regional study of the deepwater portion of the Gulf of Papua, Papua New Guinea (PNG), indicates a number of large structures at a variety of stratigraphic levels that are capable of holding significant volumes of hydrocarbons. The main structural elements east of the Fly River Platform the Pandora Ridge, Pandora Trough, Aure Trough, Port Moresby Trough and the northern portion of the Eastern Plateau were established during the Paleozoic and further enhanced by Late Cretaceous to Early Paleocene Coral Sea rifting in the southeast. Structuring in the region is mostly basement involved and extensional, and is overprinted by a later compressional pulse. Extensional and compressional regimes produce many potential traps. To date, exploration in the Gulf of Papua has been sporadic and mainly focussed in shallow water depths. The new reprocessed seismic data indicate the following Paleozoic to Recent plays, some of which contain multiple reservoir-seal pairs, sourced by non-marine and marine source rocks:extensional Paleozoic rift fault blocks;Upper Jurassic to Lower Cretaceous turbidites (Iagifu- Hedina-Toro sandstone equivalents);Campanian to Middle Paleocene Coral Sea synrift sandstone and basin floor fan equivalents (Pale/Barune Formations and equivalents);Middle Paleocene break-up unconformity fault blocks and intra-basinal highs;Upper Paleocene to Lower Eocene Pima Sandstone equivalent associated with the Middle Paleocene uplift and erosion;Oligocene to Lower Miocene lowstand deltas and turbidites;Miocene to Recent biohermal build-ups (possibly including a new limestone high, the Box Ridge, in front of the Pandora Ridge); Karstified Darai Limestone equivalent sealed by Aure Beds claystones;Miocene to Recent lowstand deltas and turbidites;Eocene to Pliocene stratigraphic onlaps flanking main structural highs; and,compressional plays associated with the Pliocene to Recent collision of the PNG and Pacific plates.

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26

Urwin, Chris, Quan Hua e Henry Arifeae. "COMBINING ORAL TRADITIONS AND BAYESIAN CHRONOLOGICAL MODELING TO UNDERSTAND VILLAGE DEVELOPMENT IN THE GULF OF PAPUA (PAPUA NEW GUINEA)". Radiocarbon 63, n. 2 (28 gennaio 2021): 647–67. http://dx.doi.org/10.1017/rdc.2020.145.

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ABSTRACTWhen European colonists arrived in the late 19th century, large villages dotted the coastline of the Gulf of Papua (southern Papua New Guinea). These central places sustained long-distance exchange and decade-spanning ceremonial cycles. Besides ethnohistoric records, little is known of the villages’ antiquity, spatiality, or development. Here we combine oral traditional and 14C chronological evidence to investigate the spatial history of two ancestral village sites in Orokolo Bay: Popo and Mirimua Mapoe. A Bayesian model composed of 35 14C assays from seven excavations, alongside the oral traditional accounts, demonstrates that people lived at Popo from 765–575 cal BP until 220–40 cal BP, at which time they moved southwards to Mirimua Mapoe. The village of Popo spanned ca. 34 ha and was composed of various estates, each occupied by a different tribe. Through time, the inhabitants of Popo transformed (e.g., expanded, contracted, and shifted) the village to manage social and ceremonial priorities, long-distance exchange opportunities and changing marine environments. Ours is a crucial case study of how oral traditional ways of understanding the past interrelate with the information generated by Bayesian 14C analyses. We conclude by reflecting on the limitations, strengths, and uncertainties inherent to these forms of chronological knowledge.

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27

Matsuoka, Tatsuro, e Ting T. Kan. "Passive Exclusion of Finfish by Trawl Efficiency Device(TED) in Prawn Trawling in Gulf of Papua, Papua New Guinea." NIPPON SUISAN GAKKAISHI 57, n. 7 (1991): 1321–29. http://dx.doi.org/10.2331/suisan.57.1321.

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28

Wei, Emily A., Neal W. Driscoll e Rudy L. Slingerland. "Oceanographic currents, differential subsidence, and physiography control three-dimensional clinothem growth in the Gulf of Papua, Papua New Guinea". Marine Geology 407 (gennaio 2019): 164–80. http://dx.doi.org/10.1016/j.margeo.2018.10.012.

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29

Garrett, Rhiannon, Gilles Brocard, Tristan Salles e Patrice Rey. "Constraining Upland Erodibility in Catchments Delivering Sediment to The Gulf of Papua". ASEG Extended Abstracts 2018, n. 1 (dicembre 2018): 1. http://dx.doi.org/10.1071/aseg2018abp015.

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30

McKinnon, A. D., J. H. Carleton e S. Duggan. "Pelagic production and respiration in the Gulf of Papua during May 2004". Continental Shelf Research 27, n. 12 (luglio 2007): 1643–55. http://dx.doi.org/10.1016/j.csr.2007.01.026.

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31

Moses, I., S. Main, R. J. Commons, B. Robertson, A. Mek e M. Gale. "A retrospective study of tuberculosis outcomes in Gulf Province, Papua New Guinea". Public Health Action 9, n. 1 (21 settembre 2019): S38—S42. http://dx.doi.org/10.5588/pha.18.0069.

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32

THANGAVELU, ANBARASU, BRUNO DAVID, BRYCE BARKER, JEAN-MICHEL GENESTE, JEAN-JACQUES DELANNOY, LARA LAMB, NICK ARAHO e ROBERT SKELLY. "Morphometric analyses ofBatissa violaceashells from Emo (OAC), Gulf Province, Papua New Guinea". Archaeology in Oceania 46, n. 2 (luglio 2011): 67–75. http://dx.doi.org/10.1002/j.1834-4453.2011.tb00100.x.

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33

Jones, Graham B., e Anne J. Trevena. "The influence of coral reefs on atmospheric dimethylsulphide over the Great Barrier Reef, Coral Sea, Gulf of Papua and Solomon and Bismarck Seas". Marine and Freshwater Research 56, n. 1 (2005): 85. http://dx.doi.org/10.1071/mf04097.

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Marked regional differences in dissolved dimethylsulphide (DMS), atmospheric DMS and DMS flux were recorded during July 1997 through the northern Great Barrier Reef, Coral Sea, Gulf of Papua, Solomon and Bismarck Seas. Highest concentrations of dissolved DMS occurred in the Coral Sea, Gulf of Papua and Bismarck Sea, with lower concentrations in the Great Barrier Reef and Solomon Sea. Elevated levels of atmospheric DMS often occurred in south-easterly to southerly trade winds sampled in the region 18°32′–8°12′S to 145°–151°E, where the highest biomass of coral reefs occurred. Atmospheric DMS often increased in the day after low tides and was positively correlated with tidal height in the northern Great Barrier Reef (r = 0.91, P < 0.05). For tides less than 1.6 m, atmospheric DMS increased on the rising tide for the northern GBR and NW Coral Sea (r = 0.66; P < 0.05) and for the whole voyage (r = 0.25; P < 0.05). As coral reefs have been identified as significant sources of DMS, it is suggested that the daytime increase in atmospheric DMS over much of the study area was mainly a result of high winds and extremely low tides in July, which exposed the reefs during the day.

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34

Georges, Arthur, Erika Alacs, Matthew Pauza, Felix Kinginapi, Amos Ona e Carla Eisemberg. "Freshwater turtles of the Kikori Drainage, Papua New Guinea, with special reference to the pig-nosed turtle, Carettochelys insculpta". Wildlife Research 35, n. 7 (2008): 700. http://dx.doi.org/10.1071/wr07120.

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A survey of the Kikori River drainage of the Gulf Province of Papua New Guinea identified four species of freshwater turtle. The pig-nosed turtle Carettochelys insculpta and the southern New Guinea soft-shelled turtle Pelochelys bibroni are riverine species. The New Guinea spotted turtle Elseya novaeguineae lives primarily in the tidal freshwater creeks and streams, flooded sinkholes and swamps of the lowland rainforest. The New Guinea painted turtle Emydura subglobosa resides almost exclusively in forest sinkholes and swamps. Pelochelys bibroni was the least-common species, and is probably locally endangered. Greatest turtle diversity occurred in the Karst Plains of the Kikori sub-basin, where there is a greater diversity of habitat available to turtles. Lowest diversity occurred in the highlands, where turtles were present in very low density as introduced populations, brought in from the Kikori lowlands, Mount Bosavi and the Western Province by visiting relatives. Linguistic diversity concurred with turtle diversity of the regions in which the languages were spoken. C. insculpta nests both on riverine sand beaches and on coastal beaches, sand spits and isolated sand bars where the Kikori River discharges into the Gulf of Papua. Adult females and eggs of C. insculpta are harvested heavily by local people for local consumption.

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35

Frusher, SD, D. Gwyther e R. Lindholm. "Growth of the banana prawn, Penaeus merguiensis De Man, as estimated from tagging studies in the Gulf of Papua". Marine and Freshwater Research 36, n. 6 (1985): 793. http://dx.doi.org/10.1071/mf9850793.

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To estimate the growth parameters of the banana prawn, P. merguiensis, a tag-recapture study, using vinyl streamer tags (Floy FTSL-731, was undertaken throughout the northern Gulf of Papua. Recapture data were analysed using Fabens' derivation of the von Bertalanffy growth curve. A differential growth rate was found between male and female banana prawns: L∞ and K values for males were 29.34 mm carapace length (C.L.) and 0.136 per week, and for females 35.34 mm C.L. and 0.117 per week, respectively. The assumptions applied in estimating the parameters by the Fabens method were not invalidated. These prawns were shown to have a smaller maximum size than banana prawns from the Gulf of Carpentaria, and it is proposed that two discrete populations exist.

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36

Surbakti, Suriani Br. "Analisis Filogeni Thiaridae (Mollusca: Gastropoda) Papua Menggunakan Karakter Morfologi". JURNAL BIOLOGI PAPUA 4, n. 1 (14 ottobre 2018): 8–18. http://dx.doi.org/10.31957/jbp.530.

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The characteristics morphology and variations of shell can be used to reconstruct the sequence and phylogenetic of Thiaridae. 34 characters and 2 outgroups of Bellamya sp. from Papua and Sulawesi were used to observe 27 species Thiaridae. Phylogenetic Analysis Using Parsimony (PAUP Software Version 4.0., Swofford) and the neighbour joining cladogram were used to reconstruct the phylogenetic relationship and to group the taxa of Thiaridae based on distribution areas of genera separately. The study indicated that the taxon of Thiaridae can be groupped into 3 clades. Each clade depicts the taxon population based on their distribution areas in Batanta Island, Sorong, Manokwari, and Bintuni Gulf. All molded into one clade. Biak, Supiori, Serui, Wamena, Merauke, and Jayapura are formed one clade. Thiara, Terebia, and Melanoides are genera which formed a clade each genus. While Stenomelania molded into 3 clades. Morphology character and closed regionsof distribution tended to form ingroup clade and sister species.Key words: characters, phylogeni, Thiaridae, dan Papua.

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37

Galewsky, Joseph, Eli A. Silver, Christina D. Gallup, R. L. Edwards e Donald C. Potts. "Foredeep tectonics and carbonate platform dynamics in the Huon Gulf, Papua New Guinea". Geology 24, n. 9 (1996): 819. http://dx.doi.org/10.1130/0091-7613(1996)024<0819:ftacpd>2.3.co;2.

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38

MOFFAT, IAN, BRUNO DAVID, BRYCE BARKER, ALOIS KUASO, ROBERT SKELLY e NICK ARAHO. "Magnetometer surveys in archaeological research in Papua New Guinea: Keveoki 1, Gulf Province". Archaeology in Oceania 46, n. 1 (aprile 2011): 17–22. http://dx.doi.org/10.1002/j.1834-4453.2011.tb00095.x.

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39

Tomkins, Helene, Daniel Rosendahl e Sean Ulm. "Tropical Archaeology Research Laboratory Comparative Fish Reference Collection: Developing a resource for identifying marine fish remains in archaeological deposits in tropical Australasia". Queensland Archaeological Research 16 (17 marzo 2013): 1. http://dx.doi.org/10.25120/qar.16.2013.220.

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This paper outlines the methods adopted for creating a fish osteological reference collection for tropical Australasia. This collection currently contains bones from 52 fish representing 35 different species found in the Gulf of Carpentaria, Australia. This developing collection has become a valuable resource for zooarchaeological analyses in the Queensland, Torres Strait and Papua New Guinea tropical coastal zone. Ongoing development of the collection to include specimens from a wider geographic area will further support fish bone research across the region.

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40

Evans, C. R., L. J. Opnai e B. D. Kare. "Fishery ecology and oceanography of the prawn Penaeus merguiensis (de Man) in the Gulf of Papua: estimation of maximum sustainable yield and modelling of yield, effort and rainfall". Marine and Freshwater Research 48, n. 3 (1997): 219. http://dx.doi.org/10.1071/mf94222.

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Annual fishing effort for banana prawns, Penaeus merguiensis (de Man), in the Gulf of Papua increased from low levels in 1974 to around the optimum level in 1978 and peaked at 95000 trawl-hours in 1989 before decreasing after the introduction of effort controls in 1988. Maximum sustainable yield of P. merguiensis was estimated at 559 ± s.e. 25 t (of tails) by linear regression of CPUE (U) on effort using the Schaeffer model. Optimum effort was estimated at 84·0 (± s.e. 11·8) 103 trawl-hours, and an equation for the yield (CE) for a given effort (E) was derived as CE = 13·5E – (8·31 10-2)E2. Application of the CLIMPROD program to Gulf of Papua yield and effort and seasonal rainfall inputs resulted in validated modelling of the fishery. CLIMPROD selected a Schaeffer model for the CPUE–effort relationship (U = a + bE). When CLIMPROD incorporated rainfall (V), the model used was = UaV(b+c) + dV(2b)E (linear–exponential–exponential), where rainfall influences abundance and catchability. For 1974–93 overall, effort was by far the chief determinant of yield. The model using regionally averaged total rainfall in the fourth quarter and unstandardized effort data explained only an extra 5% of the variation in the following year’s catch over the model using effort alone. Standardization of effort data by 3% probably approximates the real effort applied more accurately than does recorded effort.

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41

Jablonski, Dariusz, e Mark Ballesteros. "New Regional Data and Advances in Understanding of the Stratigraphy, Tectonics, Structure and Prospectivity of the Gulf of Papua (Papua New Guinea)". ASEG Extended Abstracts 2018, n. 1 (dicembre 2018): 1. http://dx.doi.org/10.1071/aseg2018abt7_4a.

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42

Thomas, Marie Louise, David T. Pocknall, Sophie Warny, Samuel J. Bentley, Andre W. Droxler e Charles A. Nittrouer. "Assessing palaeobathymetry and sedimentation rates using palynomaceral analysis: a study of modern sediments from the Gulf of Papua, offshore Papua New Guinea". Palynology 39, n. 3 (6 maggio 2015): 410–33. http://dx.doi.org/10.1080/01916122.2015.1014526.

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43

Shinomiya, S., S. Shinomiya e K. Sakai. "A review of the genus Batepenaeopsis, with the description of a new species, B. moresbyensis sp. nov. (Decapoda, Penaeidae)". Crustaceana 89, n. 4 (2016): 495–513. http://dx.doi.org/10.1163/15685403-00003537.

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The genusParapenaeopsisAlcock, 1901 was divided into eight genera by grouping the species included, based on generic features, underAlcockpenaeopsis,Arafurapenaeopsis,Batepenaeopsis,Ganjampenaeopsis,Holthuispenaeopsis,Kishinouyepenaeopsis,Mierspenaeopsis,Parapenaeopsis(then sensu nov.) (Sakai & Shinomiya, 2011a, b). The genusBatepenaeopsisSakai & Shinomiya, 2011 is currently known to include two species,B. tenella(Spence Bate, 1888) andB. venusta(De Man, 1907). However, in the present paperP. acclivirostrisAlcock, 1905 from the Persian Gulf near Kuwait, and a new species,B. moresbyensissp. nov. from the Central Province, Port Moresby, Papua New Guinea, are presented as new members of the genusBatepenaeopsisSakai & Shinomiya, 2011.

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44

Schreyer, Christine. "Community consensus and social identity in alphabet development". Written Language and Literacy 18, n. 1 (12 febbraio 2015): 175–99. http://dx.doi.org/10.1075/wll.18.1.08sch.

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In the Huon Gulf area of Papua New Guinea, the indigenous language Jabêm was one of the languages of first contact for Lutheran German Missionaries, circa 1900. As a result, Jabêm became a language of the church and, later, a language of education. In both domains, written materials were commonly produced and generations of children were schooled in Jabêm rather than their own mother tongues. This paper discusses the relationship between Jabêm and Kala, an indigenous language spoken in six villages along the Huon Gulf Coast. Kala was without a standard orthography until recent collaborations between members of the communities and researchers from UBC Okanagan. This paper, therefore, also describes the development of the Kala standardized orthography and examines the distinct influences Jabêm has in both spoken and written domains. For instance, Jabêm’s role as a written authority retains positive connotation, which influenced the newly created Kala orthography.

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45

Walsh, J. P., e C. A. Nittrouer. "Mangrove-bank sedimentation in a mesotidal environment with large sediment supply, Gulf of Papua". Marine Geology 208, n. 2-4 (agosto 2004): 225–48. http://dx.doi.org/10.1016/j.margeo.2004.04.010.

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46

Tcherepanov, Evgueni N., André W. Droxler, Philippe Lapointe, Kenneth Mohn e Odd A. Larsen. "Siliciclastic influx and burial of the Cenozoic carbonate system in the Gulf of Papua". Marine and Petroleum Geology 27, n. 2 (febbraio 2010): 533–54. http://dx.doi.org/10.1016/j.marpetgeo.2009.09.002.

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47

Wolanski, E., e D. M. Alongi. "A hypothesis for the formation of a mud bank in the Gulf of Papua". Geo-Marine Letters 15, n. 3-4 (settembre 1995): 166–71. http://dx.doi.org/10.1007/bf01204459.

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48

Davies, Peter. "Nutrient processes and chlorophyll in the estuaries and plume of the Gulf of Papua". Continental Shelf Research 24, n. 19 (dicembre 2004): 2317–41. http://dx.doi.org/10.1016/j.csr.2004.07.012.

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49

DAVID, BRUNO, ANDREW FAIRBAIRN, KEN APLIN, LESLEY MUREPE, MICHAEL GREEN, JOHN STANISIC, MARSHALL WEISLER et al. "OJP, a terminal Pleistocene archaeological site from the Gulf Province lowlands, Papua New Guinea". Archaeology in Oceania 42, n. 1 (aprile 2007): 31–33. http://dx.doi.org/10.1002/j.1834-4453.2007.tb00013.x.

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50

Plato, C. C., H. A. Brown e D. C. Gajdusek. "The dermatoglyphics of the Elema people from the Gulf district of Papua New Guinea". American Journal of Physical Anthropology 42, n. 2 (2 maggio 2005): 241–50. http://dx.doi.org/10.1002/ajpa.1330420212.

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