Music and movement: A comparative study between the BAPNE and Suzuki Methods

The aim of this article is to compare the Suzuki and BAPNE methods based on bibliography published for both approaches. In the field of musical and instrumental education and especially for the childhood stage, the correct use of the body and voice are of fundamental importance. These two methods differ from one another; one principally musical and instrumental, which is the Suzuki method, and one non-musical, the BAPNE method, which aims at stimulating attention, concentration, memory and the executing function of the pupil through music and body percussion. Comparing different approaches may provide teachers with a useful insight for facing different issues related to their discipline.

Agreement between William Croswell and Charles Turner, 1807 September

Draft of an agreement between Croswell and Turner related to their evening school in Liverpool.

Bond between John Leverett and Elisha Cooke to John White, Treasurer of Harvard College, 1716 November 20

Two folio-sized leaves containing a one-and-a-half page copy of the bond between John Leverett and Elisha Cooke to John White, Treasurer of Harvard, for £200. The bond was witnessed by William Austin and Mary Gilbert. An October 3, 1726 receipt of payment from Nathaniel Byfield on the bond, signed by Treasurer Edward Hutchinson, is located on the verso of the first leaf.

Bond between John Leverett and Edward Hutchinson, Treasurer of Harvard College, 1722 June 13

One-folio sized leaf containing a handwritten copy of a bond between John Leverett and Edward Hutchinson, Treasurer of Harvard. The bond was witnessed by Benjamin Walker and John Edwards, Jr. An October 3, 1726 receipt of payment from Nathaniel Byfield on the bond, signed by Treasurer Edward Hutchinson, is located on the verso of the first leaf.

Agreement between John Lowell and John Walton, Thomas Mason, Joseph Holmes, and Samuel Mason to finish the basement of University Hall, 7 June 1814

This contract includes stipulations for finishing the two kitchens, windows, and floors in University Hall by the first of August 1815.

Surveyors' division of Kittery farm between Nicholas Shapleigh and John Shapleigh, Jan. 12, 1739/40, with paper wrapper from 1798

Paper wrapper reads: "Nicholas Shapleigh & John Shapleigh / Division of farm at Kittery / Recorded January 31st, 1798 / 17 cents duty." The legal document establishing the division of the land is signed by each of the three surveyors: Nicholas Morrell(?), William Fry, and Daniel Emery.

[Power of attorney between Stephen Sewall and Thomas Wigglesworth], 1794 August 21

This one-page printed form appoints Thomas Wigglesworth as the "true and lawful Attorney" for Stephen Sewall. The form is notarized by Samuel Barrett and witnessed by Barrett and his daughter Peggy Barrett.

Opinions filed by the commissioners acting under the VII. article of the Treaty of Amity Commerce and Navigation between Great Britain and the United States of America : manuscript, 1797-1799

Opinions concerning the 7th article of the treaty.

[Deed between William Porter and Oliver Hildrith], 1808 March 31

Printed land deed between grantor William Porter, a brick-layer, and grantee Oliver Hildrith, a cordwainer, for a lot of land on Winsor street in Cambridge.

Indenture between William Tudor and Williams, Jones & Co.,

Document outlining terms and conditions of Tudor employment as manager of the Birmingham nail factory.

The Commerce between Nova Scotia and the United States, undated

Undated essay regarding the state of commerce between the United States and Nova Scotia, including specific mentions of foodstuffs traded. Docketed by a letter, likely to a publisher, explaining Tudor’s belief that trade with the United States is beneficial to Nova Scotia and should be encouraged by Great Britain.

The petitioners for settling His Majesties lands and islands lying between Nova Scotia and the province of Main in New England in America : manuscript, [ca. 1720]

Written in an unidentified hand, signed by Barkstead.

Stable isotope record of foraminifera from South Atlantic sediments with reconstruction of paleotemperatures and paleosalinities

Changes in surface water hydrography in the Southern Ocean (eastern Atlantic sector) could be reconstructed on the basis of isotope-geochemical and micropaleontological studies. A total of 75 high quality multicorer sediment surface samples from the southern South Atlantic Ocean and three Quaternary sediment cores, taken on a meridional transect across the Antarctic Circumpolar Current, have been investigated. The results of examining stable oxygen isotope compositions of 24 foraminiferal species and morphotypes were compared to the near-surface hydrography. The different foraminifera have been divided into four groups living at different depths in the upper water column. The 8180 differences between shallow-living (e.g. G. bulloides, N. pachyderma) and deeper-dwelling (e. g. G. inflata) species reflect the measured temperature gradient of the upper 250 m in the water column. Thus, the 6180 difference between shallow-living and deeper-living foraminifera can be used as an indicator for the vertical temperature gradient in the surface water of the Antarctic Circumpolar Current, which is independent of ice volume. All planktonic foraminifera in the surface sediment samples have been counted. 27 species and morphotypes have been selected, to form a reference data Set for statistical purposes. By using R- and Q-mode principal component analysis these planktonic foraminifera have been divided into four and five assemblages, respectively. The geographic distribution of these assemblages is mainly linked to the temperature of sea-surface waters. The five assemblages (factors) of the Q-mode principal component analysis account for 97.l % of the variance of original data. Following the transferfunction- technique a multiple regression between the Q-mode factors and the actual mean sea-surface environmental parameters resulted in a set of equations. The new transfer function can be used to estimate past sea-surface seasonal temperatures for paleoassemblages of planktonic foraminifera with a precision of approximately ±1.2°C. This transfer function F75-27-5 encompasses in particular the environmental conditions in the Atlantic sector of the Antarctic Circumpolar Current. During the last 140,000 years reconstructed sea-surface temperatures fluctuated in the present northern Subantarctic Zone (PS2076-1/3) at an amplitude of up to 7.5°C in summer and of up to 8.5°C in winter. In the present Polarfrontal Zone (PS1754-1) these fluctuations between glacials and interglacials show lower temperatures from 2.5 to 8.5°C in summer and from 1.0 to 5.0°C in winter, respectively. Compared to today, calculated oxygen isotope temperature gradients in the present Subantarctic Zone were lower during the last 140,000 years. This is an indicator for a good mixing of the upper water column. In the Polarfrontal Zone also lower oxygen isotope temperature gradients were found for the glacials 6, 4 and 2. But almost similar temperature gradients as today were found during the interglacial stages 5, 3 and the Holocene, which implicates a mixing of the upper water column compared to present. Paleosalinities were reconstructed by combining d18O-data and the evaluated transfer function paleotemperatures. Especially in the present Polarfrontal Zone (PS1754-1) and in the Antarctic Zone (PS1768-8), a short-term reduction of salinity up to 4 %o, could be detected. This significant reduction in sea-surface water salinity indicates the increased influx of melt-water at the beginning of deglaciation in the southern hemisphere at the end of the last glacial, approximately 16,500-13,000 years ago. The reconstruction of environmental Parameters indicates only small changes in the position of the frontal Systems in the eastern sector of the Antarctic Circumpolar Current during the last 140,000 years. The average position of the Subtropical Front and Subantarctic Front shifted approximately three latitudes between interglacials and glacials. The Antarctic Polar Front shifted approximately four latitudes. But substantial modifications of this scenario have been interpreted for the reconstruction of cold sea-surface temperatures at 41Â S during the oxygen isotope stages 16 and 14 to 12. During these times the Subtropical Front was probably shified up to seven latitudes northwards.