Oesterreich's Obstbau auf der Triester Export-Ausstellung 1882, veranstaltet durch den Oesterreichischen Pomologen-Verein. Eine Studie mit besonderer Berucksichtigung der Alpenlander, von Heinrich, Graf v. Attems. 2. Aufl.

Mode of access: Internet.

Heinrich Rebau's Naturgeschichte für schule und haus. Eine gemeinfassliche und ausfünrliche beschrelbung aller drei reiche der natur

Mode of access: Internet.

Regulation of trade in drugs: hearings, Ninety-first Congress, second session, on S. 1575, to regulate trade in drugs and devices by prohibiting the dispensing of drugs or devices by medical practitioners and their participation in profits from the dispensing of such products, except under certain circumstances, and for other purposes, June 16 and 17, 1970.

"Serial no. 91-81."

Heinrich Heine's Sämmtliche Werke.

Edited by Becker.

Sitzungsberichte der Heidelberger Akademie der Wissenschaften, Stiftung Heinrich Lanz, Philosophisch-Historische Klasse.

Vols. for 1910-1923 called also bd. 1-14.

Heinrich von Treitschke und die preussisch-deutsche Frage von 1860-1866 : ein Beitrag zur Entwicklung von Treitschkes politischen Anschauungen

von Hildegard Katsch

La distinction épistémologique entre sciences de la culture et sciences de la nature chez Heinrich Rickert

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

La distinction épistémologique entre sciences de la culture et sciences de la nature chez Heinrich Rickert

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Biomarker in Heinrich event layers

There are controversies regarding the origin of Heinrich layer 3 (H3), the massive ice-rafting and meltwater event in the North Atlantic during the last glacial cycle spanning a time window between 29 and 30 kyr B.P. Some argue in favor of a Laurentide Ice Sheet source similar to other Heinrich layers, while a contending view argues for the European ice sheet source. Existing geochemical proxies such as 40Ar/39Ar, 206Pb/204Pb, or epsilon-Nd, etc., could not be used to distinguish among various sources of ice-rafted debris in H3 because of their low abundances, suggesting a background glacial sediment signal. In order to circumvent this problem a biomarker-based approach is used to characterize the provenance of H layers 2, 3, and 4 and other non-Heinrich layers. The presence of hopanes and steranes and their aromatic counterparts in the H layers is incompatible with Recent sediments and is attributed to the transportation of organic matter because of the glacial erosion of source rocks. The most diagnostic and useful signatures of this ancient organic matter in the H layers are the dominance of C34 hopanoids over C33 and the occurrence of isorenieratane along with palaerenieratane. Biomarkers signatures in H layers 2 and 3 of the Labrador Sea suggest no difference in their source. Hydrocarbon distributions suggest that these sediments were derived from the Middle to Late Ordovician and Silurian source rocks of the Hudson Bay of eastern Canada. Biomarker data of the H layer 4 from the northwest Atlantic reveal that the sediments of this layer have a similar source to the H layers in the Labrador Sea.

(Appendix A) Oxygen and carbon isotope results of detrital carbonate grains of Heinrich layers from HU90-013-028 and IODP Sites 303-U1302/U1303/U1308 in the North Atlantic Ocean

We report oxygen and carbon isotope results of detrital carbonate grains from Heinrich layers at three sites in the North Atlantic located along a transect from the Labrador Sea to the eastern North Atlantic. Oxygen isotopic values of individual detrital carbonate grains from six Heinrich layers at all sites average - 5.6 ppm ± 1.5 ppm (1sigma; n = 166), reflecting values of dolomitic limestone derived from source areas in northeastern Canada. The d18O of bulk carbonate at Integrated Ocean Drilling Program (IODP) Site U1308 (re-occupation of Deep Sea Drilling Project (DSDP) Site 609) in the eastern North Atlantic records the proportion of detrital to biogenic carbonate and d18O decreases to - 5 ppm during Heinrich (H) events 1, 2, 4 and 5 relative to a background value of ~ 1 to 2 ppm for biogenic carbonate. Bulk d18O also decreases during H3 and H6 but only attains values of - 1ppm, indicating either a greater proportion of biogenic-to-detrital carbonate or a different source. Because the d18O of detrital carbonate is ~ 9 ppm lower than foraminifer carbonate, any fine-grained detrital carbonate not removed from the inner test chambers will lower foraminifer d18O. We conclude bulk carbonate d18O is a sensitive proxy for detrital carbonate and may be useful for identifying Heinrich layers in cores within and near the margins of the North Atlantic ice-rafted detritus (IRD) belt.