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Festival of the month - CTH 591
No full textTranscription of the tablet fragments listed in the CTH 591, related to the festival of the month. Emmanuel Laroche translated this text as "Fête du mois,” and classified in the category of texts of festivals and cults among calendrical rituals (Catalogue des textes Hittites, No. 591).Paper (2 sheets
Fragments of recitations - Festival of the month - CTH 591
No full textTranscription of the tablet fragments listed in the CTH 591, related to the festival of the month. Emmanuel Laroche translated this text as "Fête du mois,” and classified in the category of texts of festivals and cults among calendrical rituals (Catalogue des textes Hittites, No. 591).Paper (1 sheet
Fragments of recitations - Festival of the month - CTH 591
No full textTranscription of the tablet fragments listed in the CTH 591, related to the festival of the month. Emmanuel Laroche translated this text as "Fête du mois,” and classified in the category of texts of festivals and cults among calendrical rituals (Catalogue des textes Hittites, No. 591).Paper (1 sheet
Accumulation rates, grain-size fractions and calcium carbonate at DSDP Sites 89-586 and 90-591
No full textCarbonate oozes recovered by hydraulic piston coring at DSDP Site 586 on Ontong-Java Plateau and Site 591 on Lord Howe Rise have carbonate contents that are consistently higher than 90% with only minor variations. Consequently, paleoceanographic signals were not recorded in detail in the carbonate contents. However, mass accumulation rates of carbonate increased in the late Miocene to mid-Pliocene, reflecting an increase in productivity, then abruptly decreased from mid-Pliocene to the present. Variations in relative abundances of coarse material (foraminifers) and fine material (mostly calcareous nannofossils) do reflect histories of current winnowing and biogenic productivity at the two sites. The late Miocene from 10.5 to 6.5 m.y. ago was a time of relatively constant, quiet, pelagic sedimentation with typical southwest Pacific sedimentation rates of 20-25 m/m.y. The average coarse-fraction abundances are always higher at Site 586 than at Site 591, which reflects winnowing at Site 586. These conditions were interrupted between 6.5 to 4.0 m.y. ago when increased upwelling at the Subtropical Divergence and the Equatorial Divergence produced greater productivity of calcareous planktonic organisms. The increased productivity is suggested by large increases in both fineand coarse-fraction material and constant ratios of foraminifers to nannofossils. The maximum of productivity was about 4.0 m.y. ago. This period of increased upwelling is coincident with the inferred development of the West Antarctic ice sheet. The high productivity was followed by an abrupt increase in winnowing about 2.5 m.y. ago at Site 591, but not until about 2.0 m.y. ago at Site 586. By 2.0 m.y. ago in the late Pliocene, quiet, pelagic sedimentation conditions prevailed, similar to those of the late Miocene. The last 0.7 m.y. has been a period of relatively intense winnowing on Lord Howe Rise but not on Ontong-Java Plateau.
The coarse-fraction data have both long- and short-period fluctuations. Long-period fluctuations at Site 591 average about 850 *10**3 yr./cycle and those at Site 586 average 430*10**3 yr./cycle. The highest amplitudes are found in the Pliocene and Quaternary sections. The short-period fluctuations range from 100 to 48*10**3 yr./cycle at Site 586 and from 250 to 33 *10**3 yr./cycle at Site 591. The effects of local fluctuations of productivity and winnowing have modified the primary orbital forcing signals at these two sites to yield complex paleoceanographic records
Resolución UNRN N° 591/2009. Aprobar la designación como docente interino
No full textFil: Universidad Nacional de Río Negro (U). Universidad Nacional de Río Negro. Río Negro, ArgentinaResolución UNRN N° 591/2009. Aprobar la designación como docente interinofals
Invocation to the mountains [Invocation à des montagnes] Festival of the month - CTH 591
No full textAnalytical translation of the tablet fragments listed in the CTH 591, related to the festival of the month. Emmanuel Laroche translated this text as "Fête du mois,” and classified in the category of texts of festivals and cults among calendrical rituals (Catalogue des textes Hittites, No. 591).Paper (1 sheet
Band 2, 591 (Sammlung Friedlaender)
No full textBAND 2, 591 (SAMMLUNG FRIEDLAENDER)
Band 2, 591 (Sammlung Friedlaender) (Public Domain) (1
(Table 2) Distribution of phytoliths in selected samples from DSDP Site 90-591
No full textPhytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regional distribution is related to the arid and semiarid regions of Australia, from where they were blown by westerly winds into the Tasman Sea area. The stratigraphic record ranges from the middle Miocene, at about 14.4 m.y., until the early Pleistocene. A distinct increase in frequencies observed during the Pliocene and a maximum at about 2.5 m.y. coincide with important trends in paleogeography and paleoclimatology: the development of the Antarctic ice cap, the northward drift of the Australian Plate, and the generation of arid conditions on the Australian continent
Going Beyond Counting First Authors in Author Co-citation Analysis
No full textThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
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