Sporocarp succession of soil-inhabiting macrofungi in an autochthonous subalpine Norway spruce forest of Switzerland

Sporocarps of macrofungi have been recorded in two neighbouring pure stands of Norway spruce (Picea abies) of different age due to a wind-throw in the subalpine zone of the Alps. The still open young stand of 30 years with trees up to 6 m displayed 80 species, the mature closed forest stand 90 species. Species richness of mycorrhizal fungi is higher in the mature stand than in the younger one, however, with an almost doubled sporocarp production in the latter one. The opposite is found with saprotrophic fungi. Several fungi appeared only in one forest type confirming the concept of early stage versus late stage fungi. Wind-throws as irregular events in subalpine forests, create gaps and add considerably to the species diversity of macrofungi.

Radionuclides in sediment cores of the Atlantic sector of the Southern Ocean

We present time series of export productivity proxy data including 230Thex-normalized deposition rates (rain rates) of 10Be, dissolution-corrected biogenic Ba, and biogenic opal as well as authigenic U concentrations which are complemented by rain rates of total (detrital) Fe and sea ice indicating diatom abundances from five sediment cores across the Atlantic sector of the Southern Ocean covering the past 150,000 years. The results suggest that 10Be rain rates and authigenic U concentration cannot serve as quantitative paleoproductivity proxies because they have also been influenced by detrital particle fluxes in the case of 10Be and bulk sedimentation rates (sediment focussing) and deep water oxygenation in the case of U. The combined results of the remaining productivity proxies of this study (rain rates of biogenic opal and biogenic Ba in those sections without authigenic U) and other previously published proxy data from the Southern Ocean (231Pa/230Th and nitrogen isotopes) suggest that a combination of sea ice cover, shallow remineralization depth, and stratification of the glacial water column south of the present position of the Antarctic Polar Front and possibly Fe fertilization north of it have been the main controlling factors of export paleoproductivity in the Southern Ocean over the last 150,000 years. An overall glacial increase of export paleoproductivity is not supported by the data, implying that bioproductivity variations in the Southern Ocean are unlikely to have contributed to the major glacial atmospheric CO2 drawdown observed in ice cores.

Sea surface temperature reconstructions of sediment cores from the Atlantic sector of the Southern Ocean

Late Quaternary summer sea surface temperatures (SSTs) have been derived from radiolarian assemblages in the East Atlantic sector of the Southern Ocean. In the subantarctic and the polar frontal zone, glacial SSTs (oxygen isotope stages 2, 4, 6, and 8) were 3°-5°C cooler than today, indicating northward displacements of the isotherms about 2°-4° of latitudes. During interglacials, SSTs almost reached modern levels (oxygen isotope stages 7 and 9) or exceeded them by 2°-3°C (oxygen isotope stages 1 and 5.5). In the subantarctic Atlantic Ocean, changes in SST and calcium carbonate content of the sediment precede variations in global ice volume in the range of the main Milankovitch frequencies. Comparisons with the timing of North Atlantic Deep Water (NADW) proxy records suggests that this early response in the subantarctic Atlantic Ocean is not triggered by the flux of NADW to the Southern Ocean.

Abundance and opal input of radiolarian species of two sediment cores from the Atlantic sector of the Southern Ocean

Radiolarian-based paleoceanographic reconstructions generally use the abundance of selected radiolarian species. However, the recent focus on the opal flux and the development of isotope measurements in biogenic opal and the organic matter embedded in it demands a better knowledge of the origin of the opal. We present here an estimation of the opal content of the skeleton of 63 radiolarian species from two sites in the Southern Ocean. The skeletons are modelled as associations of simple geometrical shapes, and the volume thus obtained is combined with opal density to obtain the amount of opal. These data are, thus, used to determine the most important opal carriers in the radiolarian assemblage in both cores.

Paleotemperature reconstructions of the Atlantic Sector of the Southern Ocean

Diatom assemblages from ODP Leg 177 sites 1093, 1094 and core PS2089-2, from the present Antarctic sea ice free zone and close to the Polar Front, were analyzed in order to reconstruct the climate development around the Mid-Brunhes Event 400 000 yr ago, as reflected by summer sea surface temperature (SSST) and sea ice distribution. Dense sample spacing allows a mean temporal resolution during Marine Isotope Stage (MIS) 11 (423-362 ka) of 300-400 yr. SSST values were estimated from diatom assemblages using a transfer function technique. The distribution pattern of sea ice diatoms indicates that the present-day ice free Antarctic Zone was seasonally covered by sea ice during the cold MIS 12 and MIS 10. These glacial periods are characterized by sea ice fluctuations with a periodicity of 3 and 1.85 kyr, suggesting the occurrence of Dansgaard-Oeschger-style millennial-scale oscillations in the Atlantic sector of the Southern Ocean during the glacial stages MIS 12 and MIS 10. Termination V (MIS 12/11) is characterized by a distinct temperature increase of 4-6°C, intersected especially at the southern site 1094 and core PS2089-2 by two distinct cooling events reminiscent of the Younger Dryas, which are associated with a northward shift of the winter sea ice edge in the Antarctic Zone. The SSST record is characterized by distinct temperature intervals bounded by stepwise, rapid changes. Maximum temperatures were reached during Termination V and the early MIS 11, exceeding modern values by 2°C over a period of 8 kyr. This pattern indicates a very early response of the Southern Ocean to global climate on Milankovitch-driven climate variability. The SSST optimum is marked by millennial-scale temperature oscillations with an amplitude of ca. 1°C and periodicities of ca. 1.85 and 1.47 kyr, probably reflecting changes in the ocean circulation system. The SSSTs during the MIS 11 temperature optimum do not exceed values obtained from other interglacial optima such as the early periods of MIS 5 or MIS 1 from the Antarctic Zone. However, the total duration of the warmest period was distinctly longer than observed from other interglacials. The comparison of the South Atlantic climate record with a high-resolution record from ODP Leg 162, site 980from the North Atlantic shows a strong conformity in the climate development during the studied time interval.

Vegetable oils of Brazil /

Mode of access: Internet.

Sugar, gold, and coffee : essays on the history of Brazil based on Francis Hull's books.

"Published as a testimonial to a great bookman [Francis Hull]"

Ports on the South Atlantic Coast of the United States : Morehead City, N. C., Brunswick, Ga., Port Everglades, Fla., Georgetown, S. C., Fernadina, Fla., Miami, Fla., Palm Beach, Fla. /

"Revision of Port series, no.16, T̀he port of Miami and Port Everglades, Fla.,' 1947; a revision, in part, of the Port series, no.12, T̀he ports of Wilmington and Morehead City, N.C.' 1950; and a revision, in part of Port series, no. 14, T̀he ports of Savannah and Brunswick, Ga.,' 1946."

A browse utilization study of big game winter ranges within the Flathead Forest of the Continental Management Unit.

Pittman-Robertson Federal Aid Project.

Address delivered before the Spanish club of Yale University, on the 15th May, 1908: The spirit of nationality in the history of Brazil, by Joaquim Nabuco ...

Cover title.

The United States of Brazil, with a chapter on the republic of Uruguay,

Mode of access: Internet.

A new and accurate history of South-America : containing a particular account of some accidents leading to the discovery of the New World, of the discovery made by Columbus, and other adventures ... : with a full description of the spanish provinces of Chili, Paraguay, and Terra Firma : of Guiana, particularly of Surinam ..., and of Cayenne belonging to the french : of Brazil, subject to the Crown of Portugal : of that part of Paraguay possessed by the Jesuits, where they have established a new monarchy ... : including the geographical, natural, political, and commercial history of every province, with the religion, manners, and customs of the inhabitants : with Dissertations on the british, spanish, portuguese, french, dutch, and indian settlements /

Sabin,

The Atlantic book of modern plays /

The Philosopher of Butterbiggens / Harold Chapin -- Spreading the news / Lady Gregory -- The Beggar and the King / Winthrop Parkhurst -- Tides / George Middleton -- Ile / Eugene O'neill -- Campbell of Kilmhor / J.A. Ferguson -- The sun / John Galsworthy -- The knave Hearts / Louise Saunders -- Fame and the poet / Lord Dunsany -- The captain of the gate / Beulah Marie Dix -- Gettysburg / Percy Mackaye -- Lonesome-Like / Harold Brighouse -- Riders of the sea / John Millington Synge -- The Land of Heart's Desire / William Butler Yeats -- The Riding to Lithend / Gordon Bottomley -- Night Watches / Allan Monkhouse -- Glory of the Morning / William Ellery Leonard -- Trifles / Susan Glaspell.

The histories of Brazil,

"Treatise on the land of Brazil in which is contained information concerning the conditions in those parts: by Pero de Maghalhães": v. 2, p. [123]-183.