@article {2119,
	title = {Drowned reefs and antecedent karst topography, Au{\textquoteright}au Channel, S. E. Hawaiian Island},
	journal = {EOS},
	volume = {83},
	year = {2002},
	note = {id: 662},
	month = {2002},
	pages = {82},
	author = {Grigg, R. W. and Grossman, E. E. and al, et}
}
@article {864,
	title = {Age and composition of carbonate shoreface sediments, Kailua Bay, Oahu, Hawaii},
	journal = {Coral Reefs},
	volume = {19},
	year = {2000},
	note = {341wmTimes Cited:32Cited References Count:43},
	month = {Jul},
	pages = {141-154},
	abstract = {The origin, age, and dynamics of carbonate sediments in Kailua Bay on Oahu, Hawaii, are described. The shoreface (from shoreline to 4 km offshore) consists of a broad (5 km(2)) fringing coral reef ecosystem bisected by a sinuous, shore-normal, sand-filled paleostream channel 200-300 m wide. The median grain diameter of surface sands is finest on the beach face (<0.3 mm) and increases offshore along the channel axis. Kailua sands are >90\% biogenic carbonate, dominated by skeletal fragments of coralline algae (e.g. Porolithon, up to 50\%) followed by the calcareous green alga Halimeda (up to 32\%), coral fragments (1-24\%), mollusc fragments (6-21\%), and benthic foraminifera (1-10\%). Sand composition and age across the shoreface are correlated to carbonate production. Corals and coralline algae, principal builders of the reef framework, are younger and more abundant in sands along the channel axis and in offshore reefal areas, while Halimeda, molluscs, and foraminifera are younger and more dominant in nearshore waters shoreward of the main region of framework building. Shoreface sediments are relatively old. Of 20 calibrated radiocarbon dates on skeletal constituents of sand, only three are younger than 500 years B.P.; six are 500-1000 years B.P.; six are 1000-2000 years B.P.; and five are 2000-5000 years B.P. Dated fine sands are older than medium to coarse sands and hence may constitute a reservoir of fossil carbonate that is distributed over the entire shoreface. Dominance of fossiliferous sand indicates long storage times for carbonate grains, which tend to decrease in size with age, such that the entire period of relative sea-level inundation (similar to 5000 years) is represented in the sediment. Despite an apparently healthy modern coral ecosystem, the surficial sand pool of Kailua Bay is dominated by sand reflecting an antecedent system, possibly one that existed under a + 1-2 m sea-level high stand during the mid- to late Holocene.},
	issn = {0722-4028},
	doi = {10.1007/s003380000085},
	author = {Harney, J. N. and Grossman, E. E. and Richmond, B. M. and Fletcher, C. H.}
}
@article {738,
	title = {Sea level higher than present 3500 years ago on the northern main Hawaiian Islands},
	journal = {Geology},
	volume = {26},
	year = {1998},
	note = {Zg996Times Cited:34Cited References Count:25},
	month = {Apr},
	pages = {363-366},
	abstract = {New data from an emerged coastal bench and associated fossil beach on Kapapa Island (Oahu), Hawaii, preserve a detailed history of middle to late Holocene sea level. These include 29 new calibrated radiocarbon ages and elevations indicating mean sea level reached a maximum position of 2.00 +/- 0.35 m ca. 3500 yr B.P. These results correlate with additional evidence from Hawaii and other Pacific islands and provide constraints on Oahu{\textquoteright}s long-term uplift rate (0.03-0.07 mm/yr), previously based solely on Pleistocene age shorelines. Our sea-level reconstruction is consistent with geophysical model predictions of Earth{\textquoteright}s geoid response to the last deglaciation and with observations of increased Antarctic ice volume during the late Holocene.},
	issn = {0091-7613},
	doi = {10.1130/0091-7613(1998)026<0363:Slhtpy>2.3.Co;2},
	author = {Grossman, E. E. and Fletcher, C. H.}
}
