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Artykuły w czasopismach na temat „Coran – Chronologie”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 11 lutego 2022

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1

Reynolds, Gabriel Said. "Le problème de la chronologie du Coran." Arabica 58, no. 6 (2011): 477–502. http://dx.doi.org/10.1163/157005811x587903.

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Abstract This study challenges the widespread scholarly assumption that the Qurʾān can only be properly understood when its suras are assigned to a chronological order based on the traditional biography of the Prophet. The first section of the study addresses the origins of this assumption, beginning with Islamic tradition and its reception in the XIXth century works of Gustav Weil and Theodor Nöldeke. The second section involves a critique of more recent defenses of the idea of a Quranic chronology. The third and final section of the article illustrates the problem of this idea by way of a co

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Shervette, Virginia R., Katherine E. Overly та Jesús M. Rivera Hernández. "Radiocarbon in otoliths of tropical marine fishes: Reference Δ14C chronology for north Caribbean waters". PLOS ONE 16, № 5 (2021): e0251442. http://dx.doi.org/10.1371/journal.pone.0251442.

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Reef fishes support important fisheries throughout the Caribbean, but a combination of factors in the tropics makes otolith microstructure difficult to interpret for age estimation. Therefore, validation of ageing methods, via application of Δ14C is a major research priority. Utilizing known-age otolith material from north Caribbean fishes, we determined that a distinct regional Δ14C chronology exists, differing from coral-based chronologies compiled for ageing validation from a wide-ranging area of the Atlantic and from an otolith-based chronology from the Gulf of Mexico. Our north Caribbean

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Hughen, Konrad A., Jonathan T. Overpeck, Scott J. Lehman, Michaele Kashgarian, John R. Southon, and Larry C. Peterson. "A New 14C Calibration Data Set for the Last Deglaciation Based on Marine Varves." Radiocarbon 40, no. 1 (1997): 483–94. http://dx.doi.org/10.1017/s0033822200018361.

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Varved sediments of the tropical Cariaco Basin provide a new 14C calibration data set for the period of deglaciation (10,000 to 14,500 years before present: 10–14.5 cal ka bp). Independent evaluations of the Cariaco Basin calendar and 14C chronologies were based on the agreement of varve ages with the GISP2 ice core layer chronology for similar high-resolution paleoclimate records, in addition to 14C age agreement with terrestrial 14C dates, even during large climatic changes. These assessments indicate that the Cariaco Basin 14C reservoir age remained stable throughout the Younger Dryas and l

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4

Richaudeau, François. "Fragments d'une chronologie de la lecture ou la longue marche vers la connaissance." Communication et langages 84, no. 1 (1990): 48–60. http://dx.doi.org/10.3406/colan.1990.2220.

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Comboul, M., J. Emile-Geay, M. N. Evans, N. Mirnateghi, K. M. Cobb, and D. M. Thompson. "A probabilistic model of chronological errors in layer-counted climate proxies: applications to annually banded coral archives." Climate of the Past 10, no. 2 (2014): 825–41. http://dx.doi.org/10.5194/cp-10-825-2014.

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Abstract. The ability to precisely date climate proxies is central to the reconstruction of past climate variations. To a degree, all climate proxies are affected by age uncertainties, which are seldom quantified. This article proposes a probabilistic age model for proxies based on layer-counted chronologies, and explores its use for annually banded coral archives. The model considers both missing and doubly counted growth increments (represented as independent processes), accommodates various assumptions about error rates, and allows one to quantify the impact of chronological uncertainties o

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Comboul, M., J. Emile-Geay, M. N. Evans, N. Mirnateghi, K. M. Cobb, and D. M. Thompson. "A probabilistic model of chronological errors in layer-counted climate proxies: applications to annually-banded coral archives." Climate of the Past Discussions 9, no. 5 (2013): 6077–123. http://dx.doi.org/10.5194/cpd-9-6077-2013.

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Abstract. The ability to precisely date climate proxies is central to the reconstruction of past climate variations. To a degree, all climate proxies are affected by age uncertainties, which are seldom quantified. This article proposes a probabilistic age model for proxies based on layer-counted chronologies, and explores its use for annually-banded coral archives. The model considers both missing and doubly-counted growth increments (represented as independent processes), accommodates various assumptions about error rates, and allows to quantify the impact of chronological uncertainties on di

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7

YOUNG, MATTHEW A. L., SIMON FOALE, and DAVID R. BELLWOOD. "The last marine wilderness: spearfishing for trophy fishes in the Coral Sea." Environmental Conservation 43, no. 1 (2015): 90–95. http://dx.doi.org/10.1017/s0376892915000272.

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SUMMARYIsolation can provide marine ecosystems with a refuge from human impacts. However, information on the biodiversity, ecology and fisheries of remote regions is often sparse. The proposed Coral Sea Marine Reserve could create one of the world's largest and most remote marine parks, yet little information is available to inform discussions. Fish captures from the Coral Sea and adjacent Great Barrier Reef (GBR) were assessed from reports contained in a chronology of spearfishing publications from 1953 to 2009, and reveal for the first time the history of recreational spearfishing in the Cor

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Gulliver, Pauline, Suzanne Palmer, Chris Perry, and Scott Smithers. "Are Coral Clasts from a Turbid Near-Shore Reef Environment a Suitable Material for Radiocarbon Analysis?" Radiocarbon 55, no. 2 (2013): 624–30. http://dx.doi.org/10.1017/s0033822200057775.

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Use of coral skeletons to determine growth histories of reefs situated in warm, clear tropical waters is well established. Recently, however, there has been increasing awareness of the significance of reefs occurring in environments that are considered as marginal for coral growth, such as turbid inshore settings characterized by episodes of elevated turbidity, low light penetration, and periodic sediment burial. While these conditions are generally considered as limiting for coral growth, coral reefs in these settings can exhibit high live coral cover and species diversity, and thus can be bo

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9

Weisler, Marshall I., Kenneth D. Collerson, Yue-Xing Feng, Jian-Xin Zhao, and Ke-Fu Yu. "Thorium-230 coral chronology of a late prehistoric Hawaiian chiefdom." Journal of Archaeological Science 33, no. 2 (2006): 273–82. http://dx.doi.org/10.1016/j.jas.2005.07.012.

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Skinner, L. C. "Revisiting the absolute calibration of the Greenland ice-core age-scales*." Climate of the Past 4, no. 4 (2008): 295–302. http://dx.doi.org/10.5194/cp-4-295-2008.

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Abstract. Recently, an absolute "calibration" was proposed for the GRIP and GISP2 Greenland ice-core time scales (Shackleton et al., 2004). This calibration attempted to reconcile the stratigraphic integration of ice-core, marine and speleothem archives with the absolute age constraints that marine and speleothem records incorporate. Here we revisit this calibration in light of the new layer-counted chronology of the NGRIP ice-core (GICC05). The GICC05 age-scale differs from the proposed absolute calibration by up to 1200 years late in the last glaciation, with implications both for radiocarbo

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11

Braswell, Geoffrey E. "Obsidian-Hydration Dating, the Coner Phase, and Revisionist Chronology at Copan, Honduras." Latin American Antiquity 3, no. 2 (1992): 130–47. http://dx.doi.org/10.2307/971940.

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The technique of obsidian-hydration dating contains great potentials for error, from both laboratory determinations of rate constants and measurements of effective hydration temperatures (EHTs) in the field. The rate constants used to determine these dates are of questionable validity and need to be independently verified. Significantly, no measurements of EHTs were taken at the site of Copán, Honduras, until the majority of the obsidianhydration dates were calculated. An error of but a few Kelvins in estimated EHT can lead to dates that are in error by several centuries. In view of the likeli

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Freter, AnnCorinne. "Chronological Research at Copan:Methods and implications." Ancient Mesoamerica 3, no. 1 (1992): 117–33. http://dx.doi.org/10.1017/s0956536100002340.

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AbstractAs a consequence of long-term archaeological research at Copan, 1,425 archaeological sites containing 4,507 structures have been located and mapped over an area of 135 km2. As part of the PAC II research, 200 archaeological sites representing a 15% stratified random sample of all valley sites were test excavated from 1983–1989. From these excavations, 2,150 obsidian hydration dates were processed, representing the largest number of chronometric dates from controlled contexts currently available from any southern Lowland Maya site. Based on this chronological research, there appears to

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13

Colonna, Michel, Joel Casanova, Wolf-Christian Dullo та Gilbert Camoin. "Sea-Level Changes and δ18O Record for the Past 34,000 yr from Mayotte Reef, Indian Ocean". Quaternary Research 46, № 3 (1996): 335–39. http://dx.doi.org/10.1006/qres.1996.0071.

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New sea-level and δ18O curves for the past 34,000 yr, based on uranium–thorium chronology, are proposed for the southwestern part of the Indian Ocean. The archives include cores drilled from onshore coral reefs and submersed samples from foreslope corals of Mayotte in the Comoro Islands. The Mayotte sea-level curve shows a lowstand of 145 ± 5 m below the present level during the last glacial maximum dated at 18,400 yr. This lowstand is supported by the maximum18O enrichment in the coral colonies. The residual signal (Δδ18O), controlled by sea-surface temperature changes, indicates that surface

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14

Brady, James E. "A Reassessment of the Chronology and Function of Gordon's Cave #3, Copan, Honduras." Ancient Mesoamerica 6 (1995): 29–38. http://dx.doi.org/10.1017/s095653610000208x.

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AbstractRecent excavations in the first chamber of Gordon's Cave #3 encountered a use floor with a substantial quantity of sherds and artifacts. Middle Preclassic, Gordon subphase sherds were recovered, but overall the ceramics suggest that Preclassic use of the cave was minor with the most intensive use occurring during the Classic period. The artifact assemblage provides a fuller picture of cave rituals which appear to be similar in many respects to those practiced by modern groups in the Guatemalan highlands.

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15

Taylor, F. W., Paul Mann, S. Valastro, and Kevin Burke. "Stratigraphy and Radiocarbon Chronology of a Subaerially Exposed Holocene Coral Reef, Dominican Republic." Journal of Geology 93, no. 3 (1985): 311–32. http://dx.doi.org/10.1086/628954.

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Fan, Tianlai, Kefu Yu, Jianxin Zhao, et al. "Strontium isotope stratigraphy and paleomagnetic age constraints on the evolution history of coral reef islands, northern South China Sea." GSA Bulletin 132, no. 3-4 (2019): 803–16. http://dx.doi.org/10.1130/b35088.1.

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Abstract Understanding the history of the response of coral reefs to past climate changes can provide valuable information for predicting the future response of modern reefs. However, dating such ancient biotic carbonate is still challenging because of its sensitivity to diagenetic alteration processes, scarcity of well-preserved fossils, and low magnetic mineral content. There have been a long debates about the origin and evolutionary history of coral reefs in the northern South China Sea, mainly due to the lack of direct and reliable age constraints. This provides us with a good opportunity

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17

Jöris, Olaf, and Bernhard Weninger. "Extension of the 14C Calibration Curve to ca. 40,000 Cal BC by Synchronizing Greenland 180/16O Ice Core Records and North Atlantic Foraminifera Profiles: A Comparison with U/Th Coral Data." Radiocarbon 40, no. 1 (1997): 495–504. http://dx.doi.org/10.1017/s0033822200018373.

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For a better understanding of pre-Holocene cultural history, archaeologists are in need of an absolute time scale that can be confirmed and duplicated by different dating methods. Proxy data available from archaeological sites do not, in themselves, allow much reflection on absolute age. Even when founded on supporting radiocarbon data, Paleolithic chronologies that are beyond the actual limits of 14C calibration still remain relative ones, and thus are often quite tentative. Lacking the possibility of calibration for the Paleolithic, archaeologists often attempt to correlate their data with d

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18

Ku, Teh-Lung, M. Ivanovich, and Shangde Luo. "U-Series Dating of Last Interglacial High Sea Stands: Barbados Revisited." Quaternary Research 33, no. 2 (1990): 129–47. http://dx.doi.org/10.1016/0033-5894(90)90014-c.

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AbstractU-series chronologies of the emerged coral limestone terraces on Barbados, West Indies, together with those of the terraces from New Guinea, have formed the basis for most late Pleistocene eustatic models. The so-called “Barbados sea level model” has been challenged in recent years, however. A major issue is whether during oxygen isotope stage 5e, when Rendezvous Hill reef complex on Barbados Island formed, the sea rose above the present position for one relatively brief period of <10,000 yr, or for two or more periods spanning approximately from 140,000 to 115,000 yr B.P. Evidence

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Thompson, Schmitty B., and Jessica R. Creveling. "A global database of marine isotope substage 5a and 5c marine terraces and paleoshoreline indicators." Earth System Science Data 13, no. 7 (2021): 3467–90. http://dx.doi.org/10.5194/essd-13-3467-2021.

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Abstract. In this review we compile and document the elevation, indicative meaning, and chronology of marine isotope substage 5a and 5c sea level indicators for 39 sites within three geographic regions: the North American Pacific coast, the North American Atlantic coast and the Caribbean, and the remaining globe. These relative sea level indicators, comprised of geomorphic indicators such as marine and coral reef terraces, eolianites, and sedimentary marine- and terrestrial-limiting facies, facilitate future investigation into marine isotope substage 5a and 5c interstadial paleo-sea level reco

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20

Van Houtan, Kyle S., Allen H. Andrews, T. Todd Jones, Shawn K. K. Murakawa, and Molly E. Hagemann. "Time in tortoiseshell: a bomb radiocarbon-validated chronology in sea turtle scutes." Proceedings of the Royal Society B: Biological Sciences 283, no. 1822 (2016): 20152220. http://dx.doi.org/10.1098/rspb.2015.2220.

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Some of the most basic questions of sea turtle life history are also the most elusive. Many uncertainties surround lifespan, growth rates, maturity and spatial structure, yet these are critical factors in assessing population status. Here we examine the keratinized hard tissues of the hawksbill ( Eretmochelys imbricata ) carapace and use bomb radiocarbon dating to estimate growth and maturity. Scutes have an established dietary record, yet the large keratin deposits of hawksbills evoke a reliable chronology. We sectioned, polished and imaged posterior marginal scutes from 36 individual hawksbi

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Petchey, Fiona. "New Evidence for a Mid- to Late-Holocene Change in the Marine Reservoir Effect Across the South Pacific Gyre." Radiocarbon 62, no. 1 (2019): 127–39. http://dx.doi.org/10.1017/rdc.2019.103.

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AbstractHolocene climate change in the South Pacific is of major interest to archaeologists and Quaternary researchers. Regional surface ocean radiocarbon (14C) values are an established proxy for studying changing oceanographic and climatic conditions. Unfortunately, radiocarbon variability in the marine environment over the period of specific importance to human colonization of the remote Pacific islands—the last 3500 years—has been poorly studied. In order to build robust and accurate archaeological chronologies using shell, it is important to rectify this. In this paper, radiocarbon marine

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CHEN, J. H., H. A. CURRAN, B. WHITE, and G. J. WASSERBURG. "Precise chronology of the last interglacial period: 234U-230Th data from fossil coral reefs in the Bahamas." Geological Society of America Bulletin 103, no. 1 (1991): 82–97. http://dx.doi.org/10.1130/0016-7606(1991)103<0082:pcotli>2.3.co;2.

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Fleisher, Jeffrey, Stephanie Wynne-Jones, Charlene Steele, and Kate Welham. "Geophysical Survey at Kilwa Kisiwani, Tanzania." Journal of African Archaeology 10, no. 2 (2012): 207–20. http://dx.doi.org/10.3213/2191-5784-10220.

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Geophysical survey at Kilwa Kisiwani, southern Tanzania, has recovered evidence for several aspects of town layout and the use of space within the town that enhance our understandings of this important Swahili site. Although excavations in the 1960s recovered substantial monuments at this stonetown and traced a chronology for the development of the site from the eighth to the sixteenth centuries AD, the overall site layout has remained poorly understood. This paper outlines the possibilities that geophysics creates for positioning the excavations within a broader urban landscape, and reports o

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Gass, S. E., and J. M. Roberts. "Growth and branching patterns of Lophelia pertusa (Scleractinia) from the North Sea." Journal of the Marine Biological Association of the United Kingdom 91, no. 4 (2010): 831–35. http://dx.doi.org/10.1017/s002531541000055x.

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Lophelia pertusa, a cosmopolitan cold-water coral, offers potential for new palaeoclimate proxies. This study investigated its skeletal growth patterns to aid in this development. Corallite characteristics (calyx diameter, height, thecal width and banding) of L. pertusa sampled from oil platforms in the northern North Sea were examined. The mean distance between daughter polyps along a growth axis (27.4 ± 5 mm, SD) was equivalent to the estimated annual growth rate; hence, the polyps bud once a year. The majority of growth occurred in the first year when the characteristic trumpet shape of a c

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Bastidas, C., and E. Garcı́a. "Metal Content on the Reef Coral Porites astreoides: an Evaluation of River Influence and 35 Years of Chronology." Marine Pollution Bulletin 38, no. 10 (1999): 899–907. http://dx.doi.org/10.1016/s0025-326x(99)00089-2.

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Frenkel, M. M., M. LaVigne, H. R. Miller, T. M. Hill, A. McNichol, and M. Lardie Gaylord. "Quantifying bamboo coral growth rate nonlinearity with the radiocarbon bomb spike: A new model for paleoceanographic chronology development." Deep Sea Research Part I: Oceanographic Research Papers 125 (July 2017): 26–39. http://dx.doi.org/10.1016/j.dsr.2017.04.006.

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Niespolo, Elizabeth M., Warren D. Sharp, and Patrick V. Kirch. "230Th dating of coral abraders from stratified deposits at Tangatatau Rockshelter, Mangaia, Cook Islands: Implications for building precise chronologies in Polynesia." Journal of Archaeological Science 101 (January 2019): 21–33. http://dx.doi.org/10.1016/j.jas.2018.11.001.

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Tisnérat-Laborde, Nadine, Paolo Montagna, Malcolm McCulloch, Giuseppe Siani, Sergio Silenzi та Norbert Frank. "A High-Resolution Coral-Based Δ14C Record of Surface Water Processes in the Western Mediterranean Sea". Radiocarbon 55, № 3 (2013): 1617–30. http://dx.doi.org/10.1017/s0033822200048530.

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The first high-resolution time series of pre- and post-bomb radiocarbon measurements is reported for surface waters in the western Mediterranean Sea. The Δ14C record was obtained from the aragonite skeleton of Cladocora caespitosa using a 50-yr-old corallite collected in the Ligurian Sea in 1998. Laser-ablation ICP measurements of trace elements (Li/Mg and Sr/Ca) show a strong seasonal variability, enabling the chronology of the Δ14C record to be determined at annual timescales. The mean Δ14C of pre-bomb surface water is -56 ± 3%, corresponding to a reservoir age of 262 ± 29 yr. The post-bomb

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Brachert, Thomas C., Markus Reuter, Stefan Krüger, Julia Kirkerowicz, and James S. Klaus. "Upwellings mitigated Plio-Pleistocene heat stress for reef corals on the Florida platform (USA)." Biogeosciences 13, no. 5 (2016): 1469–89. http://dx.doi.org/10.5194/bg-13-1469-2016.

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Abstract. The fast growing calcareous skeletons of zooxanthellate reef corals (z corals) represent unique environmental proxy archives through their oxygen and carbon stable isotope composition (δ18O, δ13C). In addition, the accretion of the skeleton itself is ultimately linked to the environment and responds with variable growth rates (extension rate) and density to environmental changes. Here we present classical proxy data (δ18O, δ13C) in combination with calcification records from 15 massive z corals. The z corals were sampled from four interglacial units of the Florida carbonate platform

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Gergis, J. L., and A. M. Fowler. "How unusual was late 20th century El Niño-Southern Oscillation (ENSO)? Assessing evidence from tree-ring, coral, ice-core and documentary palaeoarchives, A.D. 1525-2002." Advances in Geosciences 6 (February 1, 2006): 173–79. http://dx.doi.org/10.5194/adgeo-6-173-2006.

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Abstract. Multiple proxy records (tree-ring, coral, ice and documentary) were examined to isolate ENSO signals associated with both phases of the phenomenon for the period A.D. 1525-2002. To avoid making large-scale inferences from single proxy analysis, regional signals were aggregated into a network of high-resolution records, revealing large-scale trends in the frequency, magnitude and duration of pre-instrumental ENSO using novel applications of percentile analysis. Here we use the newly introduced coupled ocean-atmosphere ENSO index (CEI) as a baseline for the calibration of proxy records

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Sabatier, P., J. L. Reyss, J. M. Hall-Spencer, et al. "<sup>210</sup>Pb-<sup>226</sup>Ra chronology reveals rapid growth rate of <i>Madrepora oculata</i> and <i>Lophelia pertusa</i> on world's largest cold-water coral reef." Biogeosciences 9, no. 3 (2012): 1253–65. http://dx.doi.org/10.5194/bg-9-1253-2012.

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Abstract. Here we show the use of the 210Pb-226Ra excess method to determine the growth rate of two corals from the world's largest known cold-water coral reef, Røst Reef, north of the Arctic circle off Norway. Colonies of each of the two species that build the reef, Lophelia pertusa and Madrepora oculata, were collected alive at 350 m depth using a submersible. Pb and Ra isotopes were measured along the major growth axis of both specimens using low level alpha and gamma spectrometry and trace element compositions were studied. 210Pb and 226Ra differ in the way they are incorporated into coral

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Sabatier, P., J. L. Reyss, J. M. Hall-Spencer, et al. "<sup>210</sup>Pb-<sup>226</sup>Ra chronology reveals rapid growth rate of <i>Madrepora oculata</I> and <i>Lophelia pertusa</i> on world's largest cold-water coral reef." Biogeosciences Discussions 8, no. 6 (2011): 12247–83. http://dx.doi.org/10.5194/bgd-8-12247-2011.

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Abstract. Here we show the use of the 210Pb-226Ra excess method to determine the growth rate of corals from one of the world's largest known cold-water coral reef, the Røst Reef off Norway. Two large branching framework-forming cold-water coral specimens, one Lophelia pertusa and one Madrepora oculata were collected alive at 350 m water depth from the Røst Reef at ~67° N and ~9° E. Pb and Ra isotopes were measured along the major growth axis of both specimens using low level alpha and gamma spectrometry and the corals trace element compositions were studied using ICP-QMS. Due to the different

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Curtis, JS, MA Albins, EB Peebles, and CD Stallings. "Stable isotope analysis of eye lenses from invasive lionfish yields record of resource use." Marine Ecology Progress Series 637 (March 5, 2020): 181–94. http://dx.doi.org/10.3354/meps13247.

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Patterns of stable isotopes recorded in metabolically stable, serially synthesized, structures such as eye lenses can yield robust descriptions of resource use across the life histories of individual fish. We performed stable isotope analysis of eye lenses sampled from invasive lionfishes Pterois spp. and a potentially competitive native mesopredator, the graysby Cephalopholis cruentata, to compare lifelong patterns of trophic resource use on a coral reef ledge in Biscayne National Park, Florida, USA. In both lionfishes and graysby, stable isotope values increased logarithmically with eye-lens

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Douarin, Mélanie, Mary Elliot, Stephen R. Noble, et al. "Growth of north-east Atlantic cold-water coral reefs and mounds during the Holocene: A high resolution U-series and 14C chronology." Earth and Planetary Science Letters 375 (August 2013): 176–87. http://dx.doi.org/10.1016/j.epsl.2013.05.023.

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Kidwai, A. R. "The Sublime Qur'an and Orientalism." American Journal of Islam and Society 8, no. 1 (1991): 167–68. http://dx.doi.org/10.35632/ajis.v8i1.2651.

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The Qur'an, being central to both the Islamic faith and its practice, hasbeen studied in a plethora of orientalist writings-ranging from such a crudelypolemical one as Alexander Ross's English translation of the Qur'an entitledThe Alcoran of Mahomet . . . for the Satisfaction for all those who Desireto look into the Turkish Vanities (1649) to those with scholarly pretensionsand claiming to be "objective" studies, such as Noldeke's Geschichte des Qorans(1860), Goldziher's Die Richtungen der islamischen Koranauslesung (1920),Bell's The Quran translated with a Critical Rearrangement of the Surahs

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Van Cott, Donna Lee. "Melina Selverston-Scher. Ethnopolitics in Ecuador Indigenous Rights and the Strengthening of Democracy. Coral Gables: North-South Center Press, 2001. Photographs, map, chronology, bibliography, index, 152 pp.; hardcover $35, paperback $17.95." Latin American Politics and Society 44, no. 03 (2002): 170–74. http://dx.doi.org/10.1017/s1531426x00005409.

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Sajkowski, Wojciech. "Neighbourhood of the City and the Provinces in Dalmatia in the Light of Chosen Examples of Early Modern French Travel Literature." Colloquia Humanistica, no. 4 (December 31, 2015): 83–93. http://dx.doi.org/10.11649/ch.2015.005.

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Neighbourhood of the City and the Provinces in Dalmatia in the Light of Chosen Examples of Early Modern French Travel LiteratureIn early modern period Dalmatia was a region which was culturally diversified. Such cities as Zadar or Split were the centres of Italian culture, while province was a part of the Slavic world. Their location on the route to Turkey made of them a frequent stop for such French travellers as Jacob Spon (1675) or Louis-François Cassas (1782), which testimonies became a basis for printed publications. In their testimonies readers could find the information about Dalmatian

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Pirivatric, Srdjan. "Une hypothèse sur l'origine du tsar de Bulgarie Constantin Asen 'Tich'." Zbornik radova Vizantoloskog instituta, no. 46 (2009): 313–31. http://dx.doi.org/10.2298/zrvi0946313p.

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(francuski) La question de l'origine du tsar bulgare Constantin Asen (1257-1277), plus souvent appel? dans l'historiographie moderne Constantin Tich (Tih), a ?t? depuis longtemps pos?e. Les sources susceptibles d'y r?pondre sont peu nombreuses et parfaitement r?pertori?es. A commencer par Constantin Asen lui-m?me qui, dans sa charte d?livr?e au monast?re Saint-Georges pr?s de Skopje, range 'saint Simeon Nemanja, a?eul de mon empire' au nombre des anciens kt?tors de cet ?tablissement. Pour ce qui est des auteurs byzantins, chez Georges Akropolyt?s, son contemporain, ce tsar est ? plusieurs repr

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Chamera-Nowak, Agnieszka. "W sprawie edycji źródeł do historii książki polskiej." Z Badań nad Książką i Księgozbiorami Historycznymi, September 22, 2020, 5–65. http://dx.doi.org/10.33077/uw.25448730.zbkh.1985.408.

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Artykuł składa się z wypowiedzi polskich bibliologów na temat edycji źródeł do historii książki oraz jej społecznego oddziaływania. Bez dostępu do materiałów źródłowych trudno jest prowadzić i rozwijać badania bibliologiczne, które zostaną – w przyszłości – zwieńczone syntezą dziejów książki polskiej. Baza źródłowa coraz bardziej jest rozpraszana i maleje, wskutek naturalnych zniszczeń, kradzieży, różnych przeobrażeń organizacyjnych (przenoszenie i rozbicie zespołów). Swoje uwagi w sprawie konieczności podjęcia zakrojonych na szeroką skalę kwerend archiwalnych, bibliotecznych i muzealnych oraz

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Johansen, Jacob L., Lauren E. Nadler, Adam Habary, Alyssa J. Bowden, and Jodie Rummer. "Thermal acclimation of tropical coral reef fishes to global heat waves." eLife 10 (January 26, 2021). http://dx.doi.org/10.7554/elife.59162.

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As climate-driven heat waves become more frequent and intense, there is increasing urgency to understand how thermally sensitive species are responding. Acute heating events lasting days to months may elicit acclimation responses to improve performance and survival. However, the coordination of acclimation responses remains largely unknown for most stenothermal species. We documented the chronology of 18 metabolic and cardiorespiratory changes that occur in the gills, blood, spleen, and muscles when tropical coral reef fishes are thermally stressed (+3.0°C above ambient). Using representative

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Bartlett, Alison. "Ambient Thinking: Or, Sweating over Theory." M/C Journal 13, no. 2 (2010). http://dx.doi.org/10.5204/mcj.216.

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If Continental social theory emerges from a climate of intensely cold winters and short mild summers, how does Australia (or any nation defined by its large masses of aridity) function as an environment in which to produce critical theory and new knowledge? Climate and weather are intrinsic to ambience, but what impact might they have on the conditions of producing academic work? How is ambience relevant to thinking and writing and research? Is there an ambient epistemology? This paper argues that the ambient is an unacknowledged factor in the production of critical thinking, and draws on exam

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