scholarly journals Stratigraphic development and petroleum prospectivity of northern Zealandia

2021 ◽  
Author(s):  
◽  
Zelia Dos Santos
Keyword(s):  
New Zealand ◽  
Papua New Guinea ◽  
Source Rock ◽  
New Caledonia ◽  
New Guinea ◽  
Source Rocks ◽  
Reservoir Rock ◽  
Seismic Unit ◽  
Eastern Australia ◽  
Basin Floor

<p>Northern Zealandia lies between Australia, New Zealandia, and New Caledonia. It has an area of 3,000,000 km2 and is made up of bathymetric rises and troughs with typical water depths of 1000 to 4000 m. I use 39,309 line km of seismic-reflection profiles tied to recent International Ocean Discovery Program (IODP) drilling and three boreholes near the coast of New Zealand to investigate stratigraphic architecture and assess the petroleum prospectivity of northern Zealandia.  Sparse sampling requires that stratigraphic and petroleum prospectivity inferences are drawn from better-known basins in New Zealand, Australia, New Caledonia, TimorLeste and Papua New Guinea. Five existing seismic-stratigraphic units are reviewed. Zealandia Seismic Unit U3 is sampled near New Zealand and may contain Jurassic Muhiriku Group coals. Elsewhere, Seismic Unit 3 may have oil-prone equivalents of the Jurassic Walloon Coal Measure in eastern Australia; or may contain Triassic-Jurassic marine source rocks, as found in offshore Bonaparte Basin, onshore Timor-Leste, and the Papuan Basin in Papua New Guinea. Seismic Unit U2b (Mid-Cretaceous) is syn-rift and may contain coal measures, as found in Taranaki-Aotea Basin and New Caledonia. Seismic Unit U2a (Late Cretaceous to Eocene) contains coaly source rocks in the southeastern part of the study area, and may also contain marine equivalent carbonaceous mudstone, as found at Site IODP U1509. Unit U2a is transgressive, with coaly source rocks and reservoir sandstones near its base, and clay, marl and chalk above that provides a regional seal. Seismic Unit U1b (Eocene-Oligocene) is mass-transport complexes and basin floor fans related to a brief phase of convergent deformation that created folds in the southern part of the study area and regionally uplifted ridges to create new sediment source areas. Basin floor fans may contain reservoir rock and Eocene folding created structural traps. Seismic Unit U1a is Oligocene and Neogene chalk, calcareous ooze, and marl that represents overburden. Mass accumulation rates (MAR) and climatic temperatures were high in the late Miocene and early Pliocene, resulting in peak thermal maturity and hydrocarbon expulsion at ~ 3 Ma.  Approximately one-fifth of the region has adequate source rock maturity for petroleum expulsion at the base of Seismic Unit U2: Fairway Basin (FWAY), southern New Caledonia Trough (NCTS) and Reinga Basin (REIN). Plays may exist in either Seismic Unit U3 or U2, with many plausible reservoir-seal combinations, and several possible trapping mechanisms: unconformities, normal faults, folds, or stratigraphic pinch-out. The rest of the region could be prospective, but requires a source rock to exist within Seismic Unit U3, which is mostly unsampled and remains poorly understood.</p>

Stratigraphic development and petroleum prospectivity of northern Zealandia

2021 ◽  
Author(s):  
◽  
Zelia Dos Santos
Keyword(s):  
New Zealand ◽  
Papua New Guinea ◽  
Source Rock ◽  
New Caledonia ◽  
New Guinea ◽  
Source Rocks ◽  
Reservoir Rock ◽  
Seismic Unit ◽  
Eastern Australia ◽  
Basin Floor

<p>Northern Zealandia lies between Australia, New Zealandia, and New Caledonia. It has an area of 3,000,000 km2 and is made up of bathymetric rises and troughs with typical water depths of 1000 to 4000 m. I use 39,309 line km of seismic-reflection profiles tied to recent International Ocean Discovery Program (IODP) drilling and three boreholes near the coast of New Zealand to investigate stratigraphic architecture and assess the petroleum prospectivity of northern Zealandia.  Sparse sampling requires that stratigraphic and petroleum prospectivity inferences are drawn from better-known basins in New Zealand, Australia, New Caledonia, TimorLeste and Papua New Guinea. Five existing seismic-stratigraphic units are reviewed. Zealandia Seismic Unit U3 is sampled near New Zealand and may contain Jurassic Muhiriku Group coals. Elsewhere, Seismic Unit 3 may have oil-prone equivalents of the Jurassic Walloon Coal Measure in eastern Australia; or may contain Triassic-Jurassic marine source rocks, as found in offshore Bonaparte Basin, onshore Timor-Leste, and the Papuan Basin in Papua New Guinea. Seismic Unit U2b (Mid-Cretaceous) is syn-rift and may contain coal measures, as found in Taranaki-Aotea Basin and New Caledonia. Seismic Unit U2a (Late Cretaceous to Eocene) contains coaly source rocks in the southeastern part of the study area, and may also contain marine equivalent carbonaceous mudstone, as found at Site IODP U1509. Unit U2a is transgressive, with coaly source rocks and reservoir sandstones near its base, and clay, marl and chalk above that provides a regional seal. Seismic Unit U1b (Eocene-Oligocene) is mass-transport complexes and basin floor fans related to a brief phase of convergent deformation that created folds in the southern part of the study area and regionally uplifted ridges to create new sediment source areas. Basin floor fans may contain reservoir rock and Eocene folding created structural traps. Seismic Unit U1a is Oligocene and Neogene chalk, calcareous ooze, and marl that represents overburden. Mass accumulation rates (MAR) and climatic temperatures were high in the late Miocene and early Pliocene, resulting in peak thermal maturity and hydrocarbon expulsion at ~ 3 Ma.  Approximately one-fifth of the region has adequate source rock maturity for petroleum expulsion at the base of Seismic Unit U2: Fairway Basin (FWAY), southern New Caledonia Trough (NCTS) and Reinga Basin (REIN). Plays may exist in either Seismic Unit U3 or U2, with many plausible reservoir-seal combinations, and several possible trapping mechanisms: unconformities, normal faults, folds, or stratigraphic pinch-out. The rest of the region could be prospective, but requires a source rock to exist within Seismic Unit U3, which is mostly unsampled and remains poorly understood.</p>

The ultramafic—mafic complex at North Cape, northernmost New Zealand

1976 ◽  
Vol 113 (1) ◽  
pp. 61-76 ◽  
Author(s):  
M. C. Bennett
Keyword(s):  
New Zealand ◽  
Papua New Guinea ◽  
Oceanic Crust ◽  
New Caledonia ◽  
New Guinea ◽  
Quartz Diorite ◽  
Dyke Swarm ◽  
Lower Tertiary ◽  
Mafic Complex ◽  
Tectonic Belt

SummaryThe ultramafic—mafic complex at North Cape lies in a Mesozoic—Lower Tertiary tectonic belt linking New Zealand with New Caledonia and Papua New Guinea. The complex is faulted against Cretaceous submarine tholeiites and contains (1) serpentinized harzburgite and lherzolite of probable cumulus origin (and intruded by more Fe-rich wehrlitic veins and dykes), overlain by (2) layered olivine- and orthopyroxene-gabbro subvolcanic cumulates which are themselves host for (3) a sheeted dyke swarm of mainly quartz-diorite composition. It is suggested that the complex was emplaced with the Cretaceous volcanics by obduction of Mesozoic oceanic crust during the Lower Tertiary.

The genus Manota Williston (Diptera: Mycetophilidae) in Melanesia and Oceania

Zootaxa ◽  
2007 ◽  
Vol 1502 (1) ◽  
pp. 1-44 ◽  
Author(s):  
HEIKKI HIPPA
Keyword(s):  
New Species ◽  
New Zealand ◽  
Papua New Guinea ◽  
New Caledonia ◽  
Solomon Islands ◽  
New Guinea ◽  
The Other

The following new species of Manota are described: M. biunculata (Papua New Guinea), M. evexa (Papua New Guinea), M. explicans (Papua New Guinea), M. gemella (Ambon, Maluku Utara, Indonesia), M. hirsuta (Papua New Guinea), M. orthacantha (Papua New Guinea), M. parilis (Papua New Guinea), M. pentacantha (Solomon Islands), M. perissochaeta (Papua New Guinea and Solomon Islands), M. serawei (Papua New Guinea), M. sicula (Papua New Guinea), M. spathula (Papua New Guinea), M. subspathula (Papua New Guinea) and M. tricuspis (Fiji). Manota ctenophora Matile (New Caledonia), M. maorica Edwards (New Zealand) and M. taedia Matile (New Caledonia) are redescribed. Manota hamulata Colless, previously known from Palau, is redescribed and recorded from Papua New Guinea. Manota pacifica Edwards from Samoa is discussed and compared with the other species of the region. A key to the Melanesian and Oceanian species of Manota is given.

scholarly journals New stiletto flies from New Caledonia (Therevidae, Agapophytinae)

ZooKeys ◽  
2020 ◽  
Vol 984 ◽  
pp. 83-132
Author(s):  
Michael E. Irwin ◽  
Shaun L. Winterton ◽  
Mark A. Metz
Keyword(s):  
New Species ◽  
New Zealand ◽  
Papua New Guinea ◽  
New Caledonia ◽  
New Guinea ◽  
Single Species ◽  
First Record ◽  
New Genera

Stiletto-flies (Diptera: Therevidae) are highly diverse and species-rich in Australia and New Zealand, yet relatively few species have been recorded from neighbouring Papua New Guinea, Indonesia and throughout the remainder of Oceania. Indeed, in New Caledonia only a single species of the widely distributed Australasian genus Anabarhynchus Macquart (Therevinae) is previously known. Herein we describe two new agapophytine genera (i.e., Jeanchazeauiagen. nov., Calophytusgen. nov.), together comprising nine charismatic new species; this represents a first record of the subfamily from New Caledonia. The new genera and species are described and figured.

New Tectonic Reconstructions of New Guinea Derived from Biostratigraphy and Geochronology

2020 ◽  
Author(s):  
D., P. Gold
Keyword(s):  
Papua New Guinea ◽  
New Caledonia ◽  
New Guinea ◽  
Petroleum Exploration ◽  
Rift System ◽  
Zircon Age ◽  
Eastern Australia ◽  
North Eastern ◽  
West Papua ◽  
Tectonic Reconstructions

Biostratigraphic data from exploration wells in Papua, West Papua of Indonesia, Papua New Guinea and Australia were reviewed, revised and updated using modern stratigraphic interpretations. Revised stratigraphic interpretations were combined with zircon U-Pb geochronologic data to produce new tectonic reconstructions of the Indonesian provinces of West Papua and Papua. Zircon U-Pb geochronologic data used in this study include new results from the Papuan Peninsula, combined with existing datasets from West Papua, Papua New Guinea, eastern Australia and New Caledonia. Supplementary geochronologic data were used to provide independent validation of the biostratigraphic data. Findings from a compilation of biostratigraphic and zircon age data provide a framework to produce new tectonic models for the origin of New Guinea’s terranes. Two hypotheses are presented to explain observations from the biostratigraphic and geochronologic data. The ‘Allochthonous Terrane’ Model suggests that many of the terranes are allochthonous in nature and may have been derived from eastern Australia. The ‘Extended Rift’ Model suggests that the New Guinea Terranes may have been separated from north-eastern Australia by an elongate rift system far more extensive than previously described. These new tectonic models are essential for our geological understanding of the regional and can be used to drive successful petroleum exploration in this frontier area.

New black fungus gnats (Diptera: Sciaridae) from Eastern Australia

Zootaxa ◽  
2018 ◽  
Vol 4450 (2) ◽  
pp. 203
Author(s):  
WERNER MOHRIG ◽  
ELLEN KAUSCHKE ◽  
ADAM BROADLEY
Keyword(s):  
Papua New Guinea ◽  
19Th Century ◽  
Type Species ◽  
New Records ◽  
New Caledonia ◽  
New Guinea ◽  
Fungus Gnats ◽  
New Synonym ◽  
Eastern Australia ◽  
The 19Th Century

The following 17 species are described as new for science: Austrosciara heterospinata sp. n., Aus. kalliesi sp. n., Aus. multispinulata sp. n., Aus. stockerae sp. n., Aus. trichovenosa sp. n., Bradysia chloroantennata sp. n., B. fuscovirgata sp. n., B. loudoni sp. n., B. macrotrichata sp. n., B. nigroantennata sp. n., B. parareflexa sp. n., Cratyna (Peyerimhoffia) subvagabunda sp. n., Euricrium (Austroeuricrium) australiensis sp. n., Phytosciara crocera sp. n., Pseudolycoriella latostylata sp. n., Psl. rubroalata sp. n., and Scatopsciara nigrothoracica sp. n. The following 4 species are new records for Australia: B. aspercera Mohrig, B. centidens Vilkamaa, Hippa & Mohrig (both from Papua New Guinea), B. gibbosa Vilkamaa, Hippa & Mohrig and Pseudolycoriella capillosa Vilkamaa, Hippa & Mohrig (both from New Caledonia). Euricrium australiensis sp. n. is the type species of the subgenus Austroeuricrium subgen. n. First detections of the species B. conjuncta (Skuse), B. exsequialis (Skuse), B. pernitida (Skuse) and B. pictipes (Skuse) were made after their description in the 19th century. One species was declared as a new synonym: B. centidens Vilkamaa, Hippa & Mohrig, 2012 = B. mutuata Mohrig, 2016 syn. n. Five species were excluded from the subgenus Peyerimhoffia. Four are newly combined in the genus Corynoptera, crassistylata group [C. sparsula (Shi & Huang) comb. n., C. brachypoda (Shi & Huang) comb. n., C. yunnana (Shi & Huang) comb. n., C. shennongjiana (Shi & Huang) comb. n.], one in Corynoptera s. str. [C. longiprojecta (Shi & Huang) comb. n.]. Corynoptera longiprojecta (Shi & Huang) is a junior synonym of Corynoptera diversicalcaria Mohrig, 2004 from Papua New Guinea. 

scholarly journals Rhysacephala novacaledonica sp. nov. (Hymenoptera: Xiphydriidae), the first xiphydriid woodwasp from New Caledonia

Zootaxa ◽  
2007 ◽  
Vol 1516 (1) ◽  
pp. 23-30 ◽  
Author(s):  
JOHN T. JENNINGS ◽  
ANDREW D. AUSTIN ◽  
NATHAN M. SCHIFF
Keyword(s):  
New Zealand ◽  
Papua New Guinea ◽  
New Caledonia ◽  
New Guinea ◽  
First Record

Xiphydriid woodwasps have been very rarely collected in Australasia although they are widely distributed in the region. Species have been described from the Aru, Ambon and Buru Islands, Indonesia, eastern mainland Australia, Papua New Guinea, and New Zealand. Here Rhysacephala novacaledonica Jennings & Austin, sp. nov., is described, which is the first record of a xiphydriid woodwasp from New Caledonia. In addition, a key to genera for the region is presented, along with a discussion of the biology and distribution of the group in Australasia.

Revision of Coronostrongylus (Nematoda : Strongyloidea) parasitic in the stomachs of macropodid marsupials

2002 ◽  
Vol 16 (6) ◽  
pp. 893 ◽  
Author(s):  
I. Beveridge
Keyword(s):  
Papua New Guinea ◽  
Host Species ◽  
Related Species ◽  
New Guinea ◽  
Nematode Species ◽  
Closely Related Species ◽  
Nematode Genus ◽  
Eastern Australia ◽  
Wide Range ◽  
Species Occurrences

The monotypic nematode genus Coronostrongylus Johnston & Mawson, 1939 from the stomachs of macropodid marsupials was reviewed and was found to consist of a least seven closely related species. Coronostrongylus coronatus Johnston & Mawson, 1939 is found most commonly in Macropus rufogriseus, but occurs occasionally in M. dorsalis, M. parryi and Petrogale inornata. Coronostrongylus johnsoni, sp. nov. is most commonly found in M. dorsalis, but occurs also in M. rufogriseus, M. parma, Thylogale stigmatica, Petrogale godmani and P. brachyotis. Coronostrongylus barkeri, sp. nov. is most prevalent in Onychogalea unguifera, but occurs also in M. rufus, M. robustus and P. brachyotis. Coronostrongylus closei, sp. nov. is restricted to Petrogale persephone. Coronostrongylus sharmani, sp. nov. occurs only in rock wallabies from eastern Australia: P.�coenensis, P. godmani and P. mareeba; C. spratti, sp. nov. occurs in P. inornata and P. assimilis. Coronostrongylus spearei, sp. nov. is restricted to Papua New Guinea where it is found in Dorcopsulus vanhearni, Dorcopsis hageni and D. muelleri. Although all of the nematode species occur in one principal host species or a series of closely related host species, occurrences in geographically disjunct areas and in phylogenetically distant hosts are features of C. coronatus, C. barkeri, sp. nov. and C. johnsoni, sp. nov. The occurrence of seven closely related nematode species found in a wide range of macropodid host species is more readily accounted for by a hypothesis involving multiple colonisations of hosts than by the hypothesis of co-speciation.

Cochliobolus cynodontis. [Descriptions of Fungi and Bacteria].

1990 ◽  
Author(s):  
A. Sivanesan
Keyword(s):  
South Africa ◽  
Puerto Rico ◽  
New Zealand ◽  
Papua New Guinea ◽  
Geographical Distribution ◽  
Cynodon Dactylon ◽  
New Guinea ◽  
Leaf Blight ◽  
Bermuda Grass

Abstract A description is provided for Cochliobolus cynodontis. Information is included on the disease caused by the organism, its transmission, geographical distribution, and hosts. HOSTS: Cynodon dactylon (very common on this host), other Cynodon spp., Agropyron, Ammi, Arecastrum, Axonopus, Calathea, Chamaedorea, Chrysalidocarpus, Dactyloctenium, Eleusine, Hordeum, Ipomoea, Lycopersicon, Muhlenbergia, Oryza, Panicum, Pennisetum, Poa, Rhapis, Secale and Zea. DISEASE: Leafspot of Bermuda grass end other crops, leaf blight end brown patches of turf, lawns end golflinks. GEOGRAPHICAL DISTRIBUTION: Argentina, Australia, Bangladesh, Brazil, Brunei, Egypt, Ghana, Guinea, India, Israel, Iraq, Italy, Japan, Kenya, Malaysia, New Zealand, Pakistan, Papua New Guinea, Puerto Rico, Spain, South Africa, Sudan, Tanzania, Trinidad, Turkey, USA, USSR, Venezuela, Yugoslavia and Zambia. TRANSMISSION: By wind-borne conidia and seed-borne.

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