Top: Sunnyside Farm, 320 Acres, Property & Residince [sic] of Jas. B. Van Atta, Sec. 8 Salem Tp. Mich. Bottom: Res. of T. Walker, Sec.17 Salem Tp. Mich.

Salem, Mich. residences. Publication information: Chicago, Ill. : Everts & Stewart, 1874.

Qin ding Ping ding Shan Gan Xinjiang Hui fei fang lue : 320 juan.

Caption title.

Voyages de Corneille Le Brun par la Moscovie, en Perse, et aux Indes Orientales : ouvrage enrichi de plus de 320 tailles douces, des plus curieuses ... : on y a ajoûté la route qu'a suivie Mr. Isbrants, ambassadeur de Moscovie, en traversant la Russie & la Tartarie, pour se rendre à la Chine : et quelques remarques contre Mrs. Chardin & Kempfer : avec une lettre écrite à l'auteur, sur ce sujet.

Engraved frontispiece by Bernard Picart; portrait of the author engraved by G. Valck after Godfrey Kneller; other engravings unsigned.

Défense des considérations sur le célibat, relativement à la population, aux moeurs et à la politique. En réponse à la critique du célibataire anonyme, insérée dans le Journal de Paris du 24 Brumaire, an 10, no. 54, pag. 320 et 321.

Mode of access: Internet.

$320,000,000 State of Illinois general obligation refunding bonds, Illinois FIRST : series of December 2001.

"Due: October 1, as shown below."

Das moderne Landhaus, und seine innere Ausstattung : 320 Abbildungen moderner Landhäuser aus Deutschland, Österreich, England, und Finnland, mit Grundrissen und Innenräumen. Mit einleitendem Text von Hermann Muthesius.

Mode of access: Internet.

Music performance practice in the early ʻAbbāsid era 132-320 A.H./750-932 A.D. /

Includes index.

Miocene stable isotope record of IODP Site 320-U1335 and revised stable isotope record of IODP Site 321-U1337

The Miocene Climatic Optimum (MCO; ~16.9 to 14.7 Ma) provides an outstanding opportunity to investigate climate-carbon cycle dynamics during a geologically recent interval of global warmth. We present benthic stable oxygen (d18O) and carbon (d13C) isotope records (5-12 kyr time resolution) spanning the late early to middle Miocene interval (18 to 13 Ma) at Integrated Ocean Drilling Program (IODP) Site U1335 (eastern equatorial Pacific Ocean). The U1335 stable isotope series track the onset and development of the MCO as well as the transitional climatic phase culminating with global cooling and expansion of the East Antarctic ice-sheet at ~13.8 Ma. We integrate these new data with published stable isotope, geomagnetic polarity and X-ray fluorescence (XRF) scanner-derived carbonate records from IODP Sites U1335, U1336, U1337 and U1338 on a consistent, astronomically-tuned timescale. Benthic isotope and XRF scanner-derived CaCO3 records depict prominent 100 kyr variability with 400 kyr cyclicity additionally imprinted on d13C and CaCO3 records, pointing to a tight coupling between the marine carbon cycle and climate variations. Our inter-site comparison further indicates that the lysocline behaved in highly dynamic manner throughout the MCO, with >75% carbonate loss occurring at paleo-depths ranging from ~3.4 to ~4 km in the eastern equatorial Pacific Ocean. Carbonate dissolution maxima coincide with warm phases (d18O minima) and d13C decreases, implying that climate-carbon cycle feedbacks fundamentally differed from the late Pleistocene glacial-interglacial pattern, where dissolution maxima correspond to d13C maxima and d18O minima. Carbonate dissolution cycles during the MCO were, thus, more similar to Paleogene hyperthermal patterns.

Miocene stable isotope record of benthic foraminifera from IODP Site 320-U1336

Stable carbon and oxygen isotopes (d13C and d18O) of foraminiferal tests are amongst the most important tools in paleoceanography but the extent to which recrystallization can alter the isotopic composition of the tests is not well known. Here, we compare three middle Miocene (16-13 Ma) benthic foraminiferal stable isotope records from eastern equatorial Pacific sites with different diagenetic histories to investigate the effect of recrystallization. To test an extreme case, we analyzed stable isotope compositions of benthic foraminifera from Integrated Ocean Drilling Program Site U1336, for which the geochemistry of bulk carbonates and associated pore waters indicate continued diagenetic alteration in sediments > 14.7 Ma. Despite this diagenetic overprinting, the amplitudes and absolute values of the analyzed U1336 stable isotopes agree well with high resolution records from better preserved Sites U1337 and U1338 nearby. Our results suggest that although benthic foraminiferal tests of all three sites show some degree of textural changes due to recrystallization, they have retained their original stable isotope signatures. The good agreement of the benthic foraminiferal stable isotope records demonstrates that recrystallization occurred extremely rapidly (<100 kyr) after deposition. This is confirmed by the preservation of orbital cyclicities in U1336 stable isotope data and d18O values being different to inorganic calcite that would precipitate from U1336 pore waters during late recrystallization. The close similarity of the benthic foraminiferal stable isotope records between the sites allows the well resolved paleo-magnetic results of Site U1336 to be transferred to Sites U1337 and U1338 improving the global Geological Timescale.