@article {6068,
	title = {Exploring the Geology of the Central Arctic Ocean {\textendash} Understanding the Basin Features in Place and Time},
	volume = {173},
	year = {2016},
	month = {November},
	pages = {967-987},
	abstract = {<p>The history of the deep Arctic Ocean is largely unwritten. The means to understand this history may now be at hand. Bathymetry and potential field data have accumulated to the point it is possible to ask specific questions about the origins and evolution of the individual ridges and basins. The two primary basins have contrasting histories and deficits of understanding. The Eurasia Basin, formed during the Cenozoic, is well understood as far as the kinematics are concerned. The dynamics of ultraslow spreading, as observed on the Gakkel Ridge, are not well understood. It is widely thought that the Amerasia Basin formed during the Mesozoic. Most previous work has begun with a large-scale model of the basin tectonics and fit the ridges and basins it into this pattern. Enough is now known to establish the internal structure and relations from specific observations rather than a priori assumptions. This paper reviews knowledge about the central Arctic Ocean and proposes what should be done to develop a historical understanding of basin history. Ground truth from Arctic Ocean sediments is necessary. It will not be possible to establish the history of events, in geological time, until the sediments have been sampled and dated.</p>
},
	keywords = {amerasia basin, Arctic Ocean, basin features, Eurasia basin},
	doi = {10.1144/jgs2016-082  },
	url = {http://jgs.geoscienceworld.org.libproxy.unh.edu/content/173/6/967},
	author = {Coakley, Bernie and Brumley, K and Lebedeva-Ivanova, N. and David C Mosher}
}
@article {4959,
	title = {The International Bathymetric Chart of the Arctic Ocean (IBCAO) version 3.0},
	volume = {39},
	year = {2012},
	abstract = {<p>The International Bathymetric Chart of the Arctic Ocean (IBCAO) released its first gridded\&nbsp;bathymetric compilation in 1999. The IBCAO bathymetric portrayals has since supported a wide\&nbsp;range of Arctic science activities, for example, by providing constraint for ocean circulation models and the means to define and formulate hypotheses about the geologic origin of the Arctic Ocean undersea features. IBCAO Version 3.0 comprises the largest improvement since 1999 taking advantage of new data sets collected by the circum-Arctic nations, opportunistic data collected from fishing vessels, data acquired from US Navy submarines and from research ships of various nations. Built using an improved gridding algorithm, this new grid is on a 500 meter spacing, revealing much greater details of the Arctic seafloor than IBCAO 1.0 (2.5 km) and 2.0 (2.0 km). The area covered by multibeam surveys has increased from ~6 \% in Version 2.0 to ~11\% in Version 3.0.</p>
},
	keywords = {Arctic Ocean, bathymetric chart, Bathymetry grids; Arctic; Earth Sciences, ibcoa},
	author = {Martin Jakobsson and Larry A Mayer and Coakley, Bernie and Dowdeswell, J and Forbes, S. and Fridman, B. and Hodnesdal, H. and Noormets, R. and James V. Gardner and Andrew A. Armstrong and Pedersen, R. and M. Rebesco and Schenke, H-W. and Zarayskaya, Yulia and Accettella, D. and Anderson, Robert M and Bienhoff, P. and Camerlenghi, A. and Church, I and Edwards, Margo and John K Hall and Hell, B and Hestvik, O. and Kristoffersen, Yngue and Marcussen, C and Mohammad, R. and David C Mosher and Nghiem, S.V. and Pedrosa, M.T. and Travaglini, P.G. and Pauline Weatherall}
}
@article {,
	title = {Dredged Rock Samples from the Alpha Ridge, Arctic Ocean: Implications for the Tectonic History and Origin of the Amerasian Basin},
	volume = {89},
	number = {53},
	year = {2008},
	month = {Dec 15 - Dec 19},
	address = {San Francisco, CA, USA},
	keywords = {Other},
	author = {Brumley, K and Larry A Mayer and Miller, E L and Coakley, Bernie}
}
