The history of Vartan, and of the battle of the Armenians; containing an account of the religious wars between the Persians and Armenians,

"This copy was printed for Colin Macauley."

The battle of Point Pleasant; a battle of the revolution, October 10th 1774; biographical sketches of the men who participated,

Mode of access: Internet.

Robbery under law; or, The battle of the millionaires; a play in three acts and three scenes, time, 1887; treating of the adventures of the author of "Who's looney now?" by John Armstrong Chaloner.

Robbery under law.--The hazard of the die.--The temple of Apollo and the muses.--Ali Baba and the forty thieves.--The prison house.--Aladdin and his wonderful lamp.--Scorpio.--"The play's the thing."--"The shaving of Shagpat."--In re the Paris prize.--"Brer Fox and Brer Rabbit."--Isis unveiled.--Newspaper reviews [etc.]--David-up-to-date.

The battle of the Thames, in which Kentuckians defeated the British, French, and Indians, October 5, 1813, with a list of the officers and privates who won the victory,

Mode of access: Internet.

The Odyssey of Homer : with the Hymns, Epigrams, and Battle of the frogs and mice /

Mode of access: Internet.

Lays of ancient Rome: Horatius, The battle of the Lake Regillus, Virginia, The Prophecy of Capys,

Mode of access: Internet.

The select works of Jonathan Swift ... Containing the whole of his poetical works, the Tale of a tub, Battle of the books, Gulliver's travels, Directions to servants, Polite conversation, Art of punning, Miscellaneous pieces in prose, &c. ... Embellished with engravings ...

"Tale of a tub" (v. 1) and "Travels into several remote nations of the world. By Lemuel Gulliver" (v. 2) each have a special t.-p.

Benthic microalgae in coral reef sediments of the southern Great Barrier Reef, Australia

The abundance and productivity of benthic microalgae in coral reef sediments are poorly known compared with other, more conspicuous (e.g. coral zooxanthellae, macroalgae) primary producers of coral reef habitats. A survey of the distribution, biomass, and productivity of benthic microalgae on a platform reef flat and in a cross-shelf transect in the southern Great Barrier Reef indicated that benthic microalgae are ubiquitous, abundant (up to 995.0 mg chlorophyll (chl) a m(-2)), and productive (up to 110 mg O-2 m(-2) h(-1)) components of the reef ecosystem. Concentrations of benthic microalgae, expressed as chlorophyll a per surface area, were approximately 100-fold greater than the integrated water column concentrations of microalgae throughout the region. Benthic microalgal biomass was greater on the shallow water platform reef than in the deeper waters of the cross-shelf transect. In both areas the benthic microalgal communities had a similar composition, dominated by pennate diatoms, dinoflagellates, and cyanobacteria. Benthic microalgal populations were potentially nutrient-limited, based on responses to nitrogen and phosphorus enrichments in short-term (7-day) microcosm experiments. Benthic microalgal productivity, measured by O-2 evolution, indicated productive communities responsive to light and nutrient availability. The benthic microalgal concentrations observed (92-995 mg chl a m(-2)) were high relative to other reports, particularly compared with temperate regions. This abundance of productive plants in both reef and shelf sediments in the southern Great Barrier Reef suggests that benthic microalgae are key components of coral reef ecosystems.

Nd isotopes an geochemistry of bulk deep sea sediments of the Atlantic Ocean

Nd isotopes preserved in fossil fish teeth and ferromanganese crusts have become a common tool for tracking variations in water mass composition and circulation through time. Studies of Nd isotopes extracted from Pleistocene to Holocene bulk sediments using hydroxylamine hydrochloride (HH) solution yield high resolution records of Nd isotopes that can be interpreted in terms of deep water circulation, but concerns about diagenesis and potential contamination of the seawater signal limit application of this technique to geologically young samples. In this study we demonstrate that Nd extracted from the > 63 µm, decarbonated fraction of older Ocean Drilling Program (ODP) sediments using a 0.02 M HH solution produces Nd isotopic ratios that are within error of values from cleaned fossil fish teeth collected from the same samples, indicating that the HH-extractions are robust recorders of deep sea Nd isotopes. This excellent correlation was achieved for 94 paired fish teeth and HH-extraction samples ranging in age from the Miocene to Cretaceous, distributed throughout the north, tropical and south Atlantic, and composed of a range of lithologies including carbonate-rich oozes/chalks and black shales. The strong Nd signal recovered from Cretaceous anoxic black shale sequences is unlikely to be associated with ferromanganese oxide coatings, but may be derived from abundant phosphatic fish teeth and debris or organic matter in these samples. In contrast to the deep water Nd isotopic signal, Sr isotopes from HH-extractions are often offset from seawater values, suggesting that evaluation of Sr isotopes is a conservative test for the integrity of Nd isotopes in the HH fraction. However, rare earth elements (REE) from the HH-extractions and fish teeth produce distinctive middle REE bulge patterns that may prove useful for evaluating whether the Nd isotopic signal represents uncontaminated seawater. Alternatively, a few paired HH-extraction and cleaned fish teeth samples from each site of interest can be used to verify the seawater composition of the HH-extractions. The similarity between isotopic values for the HH-extraction and fish teeth illustrates that the extensive cleaning protocol applied to fish teeth samples is not necessary in typical, carbonate-rich, deep sea sediments.