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Atop its geological basement rocks, Zealandia has a drape of at least two dozen spatially separate Late Cretaceous to Holocene sedimentary basins. These typically contain 2—km-thick sequences of terrigenous and calcareous strata Zealandia Megasequence of Mortimer et al. The Zealandia Megasequence provides a Zealandia-wide stratigraphic record of continental rifting, and marine transgression events, similar to that seen in formerly conjugate east Australian basins Blewett, Continental crust varies considerably in thickness and physical properties. Christensen and Mooney give an average P wave velocity of 6.
In contrast, oceanic crust is typically 7 km thick, and, in its lower part typically has a P wave velocity of 7.
Collectively, the crustal structure results show that the rock samples of Figure 2 are not from separate continental fragments or blocks now separated by oceanic crust, but are from a single continental mass. Figure 3. Note thin continental crust in vicinity of Mesozoic arc.
Thick coastlines in Antarctica are isostatically corrected ice-free coastlines Jamieson et al. Orthographic projection.
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The thinnest crust within Zealandia is in the km-long and —km-wide New Caledonia Trough, where the water depth varies from to m Fig. This raises the question as to whether the trough is floored by oceanic crust or is a failed continental rift. Two wide-angle seismic profiles across the trough near New Caledonia Klingelhoefer et al.
Klingelhoefer et al. Sutherland et al. Where oceanic crust abuts continental crust, various kinds of continent-ocean boundaries COBs define natural edges to continents Fig. Despite its large area, Greenland is uncontroversially and correctly regarded as part of North America Figs. This is because, despite oceanic crust intervening between southern Greenland and Labrador and Baffin Island, North American continental geology is continuous across Nares Strait between northernmost Greenland and Ellesmere Island Pulvertaft and Dawes, Tectonic plate boundaries, with or without intervening oceanic crust, provide the basis for continent-continent boundaries between Africa and Eurasia, and North and South America Fig.
Large area is an inherent part of the definition of a continent sensu stricto Neuendorf et al. Cogley defined Central America 1.
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Figure 4. Note x-axis is log scale. Data mainly after Cogley except Zealandia data from Mortimer and Campbell ; microcontinents after Gaina et al.
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Emergent land area for Antarctica is the isostatically-corrected ice-free bedrock surface from Jamieson et al. New Guinea and Greenland are arbitrarily given the same submergence value as their parent continents. Discriminating between what is a continent and what is a microcontinent may be considered an arbitrary exercise. Nonetheless, maps like Figure 1 need labels. By this definition India, prior to its collision with Eurasia, would be termed a continent.
The edges of Australia and Zealandia continental crust approach to within 25 km across the Cato Trough Fig. The Cato Trough is m deep and floored by oceanic crust Gaina et al. This spatial and tectonic separation, along with intervening oceanic crust, means that the Zealandia continental crust is physically separate from that of Australia. If the Cato Trough did not exist, then the content of this paper would be describing the scientific advance that the Australian continent was 4.
It is also substantially larger than the area of the largest intraoceanic large igneous province, the Ontong Java Plateau 1. Zealandia is about the same area as greater India Figs.
Figure 4 makes a case for a natural twofold grouping of continents and microcontinents. Satellite gravity-derived bathymetry maps e. Even relatively recently, some papers refer to the offshore ridges and plateaus of Zealandia as an amalgam of continental fragments and slivers e. In contrast, we view Zealandia as a coherent, albeit thinned and stretched, continent with interconnected and throughgoing geological provinces Figs. Figure 5. Zealandia as part of the former Gondwana supercontinent. Upper panel shows Mesozoic orogen convergent margin that was active until ca.
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