This study was undertaken to explore interactions among eustatic sea level change, fluvial sediment supply, oceanic processes, and seabed morphodynamics, and their controls on delivery of terrestrial sediments to the deep sea, using the Gulf of Papua (GoP), between New Guinea and Australia, as a natural laboratory. The GoP is a 500 km wide embayment that contains excellent examples of adjacent passive and active terrestrial-oceanic margins with multiple sources of terrestrial and neritic carbonate sediments. This work examines source to sink sediment delivery from river systems to the slope and deep-sea basins of the GoP, over the last ~40 ky, at millennial temporal resolution and finer. The results offer new insights into the develo...
We investigated sediment and organic-carbon accumulation rates in two jumbo piston cores (MV-54, MV-...
Recent marine and late Pleistocene sediments examined from the Gulf of Papua (GoP), Papua New Guinea...
The island of Papua New Guinea is the result of continent-arc collision that began building the isla...
Sediment cores and geophysical data from the shelf and slope in the Pandora Trough and Gulf of Papua...
The Great Barrier Reef (GBR) margin, located on the continental margin between Papua New Guinea and ...
Geophysical and geological approaches were employed to understand sediment dispersal systems and the...
The Papua New Guinean (PNG) landscape is young and rapidly evolving, with high uplift rates and prec...
International audienceThe Gulf of Papua (GoP) has become a focal point for understanding the deposit...
Geophysical and geological approaches were employed to understand sediment dispersal systems and the...
Overtime, the north Queensland (Australia) and Gulf of Papua (Papua New Guinea) margin has been cons...
International audienceIn tropical and sub-tropical mixed siliciclastic–carbonate depositional system...
We investigated sediment and organic-carbon accumulation rates in two jumbo piston cores (MV-54, MV-...
Recent marine and late Pleistocene sediments examined from the Gulf of Papua (GoP), Papua New Guinea...
The island of Papua New Guinea is the result of continent-arc collision that began building the isla...
Sediment cores and geophysical data from the shelf and slope in the Pandora Trough and Gulf of Papua...
The Great Barrier Reef (GBR) margin, located on the continental margin between Papua New Guinea and ...
Geophysical and geological approaches were employed to understand sediment dispersal systems and the...
The Papua New Guinean (PNG) landscape is young and rapidly evolving, with high uplift rates and prec...
International audienceThe Gulf of Papua (GoP) has become a focal point for understanding the deposit...
Geophysical and geological approaches were employed to understand sediment dispersal systems and the...
Overtime, the north Queensland (Australia) and Gulf of Papua (Papua New Guinea) margin has been cons...
International audienceIn tropical and sub-tropical mixed siliciclastic–carbonate depositional system...
We investigated sediment and organic-carbon accumulation rates in two jumbo piston cores (MV-54, MV-...
Recent marine and late Pleistocene sediments examined from the Gulf of Papua (GoP), Papua New Guinea...
The island of Papua New Guinea is the result of continent-arc collision that began building the isla...