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1.
Research on brand transgressions has suggested that when a brand is involved in a transgression and perceived as harmful, consumers will punish the brand. The present research seeks to extend this literature by investigating how having a cute brand logo may reduce consumer punishment of a transgressing brand. Across five experimental studies, this research shows that a brand logo with high (vs. low) levels of cuteness associated with a transgressing brand can motivate consumers to protect the brand from harm, thus reducing consumer punishment of that brand. Notably, such motivations to protect the brand are driven by an incremental belief about the brand’s development. Moreover, the cuteness effect is attenuated in the case of repeated transgressions. Theoretical contributions to the literature on cuteness, brand logo, and brand transgression are discussed, as well as practical implications.  相似文献   
2.
The Paleogene sections of Kutch are the reference for the regional chronostratigraphic units of India. The ages of these dominantly shallow marine carbonates are mainly based on larger benthic foraminifera (LBF). The taxonomic revisions of the LBF and the progressively refined shallow benthic zonations (SBZ) have necessitated the present study on updating the stratigraphy of the area. The sedimentation in Kutch commenced with the deposition of volcaniclastics in terrestrial environments in the Paleocene. The marine transgression in SBZ 5/6 deposited finer clastics and carbonates, designated as Naredi Formation, in early Eocene. There is no evidence of marine Paleocene in Kutch. A major hiatus spanning SBZ 12 to SBZ 16 was followed by the development of a carbonate platform and deposition of Harudi Formation – Fulra Limestone during the Bartonian, SBZ 17. The hiatus corresponds to a widespread stratigraphic break in Pakistan and India to Australia, referred as the ‘Lutetian Gap.’ The Maniyara Fort Formation is assigned to SBZ 22 B and SBZ 23, and its age is revised to Chattian. Climate played a major role in building up of the Paleogene stratigraphic succession of Kutch, the carbonates formed during the warming intervals and the stratigraphic gaps were in the intervening cooling periods.  相似文献   
3.
《Sport Management Review》2019,22(4):553-565
Despite the importance of an athlete’s image and reputation as an individual brand, the academic literature lacks investigations on whether and how an athlete’s brand can be protected when they engage in unethical transgressions. Focusing on athletes’ pro-social activities, the authors presented an experimental study to test how an athlete’s pro-social efforts can alleviate negative impacts from his/her transgression. In particular, the authors test the impacts of athletes’ involvement level (high vs. low) with a pro-social cause and level of fit between an athlete and a cause (high vs. low) on sport consumers’ perceptions. Results demonstrate that an athlete’s pre-scandal charitable behaviors can mitigate adverse impact of a transgression on consumer response only when the athlete has deeply engaged in charitable behaviors. The results also show that a higher fit between an athlete and a cause can generate more severe damaging impacts on consumer evaluation than a lower fit due to consumer skepticism caused by a combination between a negative reputation and a high-fit cause.  相似文献   
4.
Several traces of biological interaction were found on penguin bones from the basal levels (Aquitanian) of the Miocene Gaiman Formation in the lower Chubut valley of the Provincia del Chubut, Argentina. The fossil-bearing beds were deposited in littoral to sublittoral environments within sediments of mostly pyroclastic origin. We interpret many traces to have been produced by predators and/or scavengers while the penguins were still in a breeding area. Many bones show cracking marks due to aerial exposure. The material is disarticulated as is usual in recent breeding areas. Potential predators were coeval terrestrial mammals, most probably marsupial carnivores. After a marine transgression, these bones were buried or exposed on the sea bottom where they could be colonized by algae, sponges, cnidarians, and other benthic organisms. We identified sponge borings in several bones. Other traces are interpreted to have been produced by echinoderms feeding on sponges or algae. No evidence of other invertebrate predators such as muricid or naticid gastropods, or decapods was found. Finally, other traces appear to have been generated by shark and possibly teleostean vertebrates feeding on epibionts. One coracoid is interpreted to have been marked by a shark that is common in the Gaiman Formation, the carcharhiniform Galeocerdo aduncus. From an ethological (Seilacherian) classification, traces on bones from the Gaiman Formation include Domichnia (sponge perforations), Praedichnia (terrestrial marsupials, sharks, teleosteans) and Pasichnia (echinoderms). Remarkably, remains of marine organisms with skeletons made of calcium carbonate are very poorly preserved in the Gaiman Formation. Only large oysters, sparse shell fragments, skeletal moulds, and bioturbation is evident. The fossil assemblage is mainly composed of phosphatic (e.g. teeth, bones, crustacean parts) and siliceous (sponge spicules, diatoms) remains.  相似文献   
5.
Diatom assemblages of sediments obtained from three sites on Kushiro Moor were analyzed to investigate the Holocene sedimentary history. The results showed that: 1) The Takkobu site was originally at the bottom of the paleo-Kushiro Bay, and after-wards the paleo-Takkobu Lagoon developed, became sealed off, and changed to a freshwater lake. The succession to peat moor probably began about 2000 yr B.P. at the Takkobu site. 2) The Tsurui site was originally at the bottom of the paleo-Kushiro Bay, then changed to the paleo-Kushiro Lagoon and became peat moor as a result of the first Holocene regression, which finished about 3600 yr B.P. The site then returned to a brackish lake again, probably due to the second Holocene transgression between 3600 and 3000 yr B.P., thereafter passing through brackish lake and freshwater lake stages, and eventually becaming peat moor at about 2000 yr B.P., 3) At the Chuo site, the second paleo-Kushiro Bay developed again as a result of the second Holocene transgression, which finished about 3000 yr B.P. Thereafter, brackish or freshwater lakes, rivers, and then peat moor developed in the central area of Kushiro Moor. 4) The second marine diatom zone (MD2 Zone), which indicates the second Holocene transgression, complete by about 3000 yr B.P., is detected only at the Chuo site in the central area of Kushiro Moor.  相似文献   
6.
As soon as Zhu Yuanzhang, the founder of the Ming Dynasty, assumed the throne, he and his Confucian assistants imposed a system of clothing regulation on the court and society in order to create a hierarchical power structure. As an important aspect of Chinese civilization, the clothing system functioned to form a social hierarchy, to regulate people’s activities, to harmonize the relations among the people, and finally to make a stable society under the close control of the state. The state control in the Ming remained effective until the reigns of Hongzhi (1488–1506) and Zhengde (1506–1521), when commercialization released people’s consumption desires and economic dynamics and caused deregulation of the Ming clothing system, which eventually undermined the state authority.  相似文献   
7.
Dance historians frequently cite the spectacular display of creaturely flight in the 1832 production of La Sylphide as one of the hallmarks of ballet Romanticism. Drawing evidence from archival sources, I argue that the ballet's staged flight of monsters—sylphs and witches—vivified a preoccupation with feminine transgression during the period known as the July Monarchy. Interpreting the witch/sylphide dyad as a response to gendered French Revolutionary discourses in politics, philosophy, literature, and medicine circulating between 1794 and 1835, I show how alterity in La Sylphide targeted the mobility of women in the public sphere as contentious and undesirable.  相似文献   
8.
Cenozoic marine strata occur in the western, eastern, and central parts of the North Patagonian Andes between ∼43°S and 44°S. Correlation of these deposits is difficult because they occur in small and discontinuous outcrops and their ages are uncertain. In order to better understand the age and sedimentary environment of these strata, we combined U–Pb (LA-MC-ICPMS) geochronology on detrital zircons with sedimentologic and paleontologic (foraminifers and molluscs) studies. Sedimentologic analyses suggest that the Puduhuapi Formation on the western flank of the Andean Cordillera was deposited in a deep-marine setting, the Vargas Formation in the central part of the Andes was deposited at outer-neritic or bathyal depths, and the La Cascada Formation on the eastern flank of the range was deposited in a shallow-marine environment. Geochronologic and paleontologic results indicate that the three marine units were deposited during the late Oligocene-early Miocene interval, although it is not clear whether this occurred during one or more marine incursions in the area. The alluvial(?) conglomeratic deposits of the La Junta Formation, exposed in the proximity of the Vargas Formation outcrops, have a maximum depositional age of ∼26 Ma and could have been deposited during the initial stage of subsidence that affected this region prior to the marine transgression over this area. The occurrence of both Pacific and Atlantic molluscan taxa in the La Cascada and Vargas formations suggests that a marine strait connected both oceans during the accumulation of these units. The new data on the age of the Puduhuapi, Vargas, and La Cascada formations indicate that these units may correlate with lower Miocene marine deposits in the forearc of central and southern Chile (Navidad Formation and equivalent units) and on the eastern flank of the Patagonian Andes (Río Foyel Formation and equivalent units). A late Oligocene−early Miocene age for these marine deposits is a reliable maximum age for the deformation and uplift of the North Patagonian Andes.  相似文献   
9.
In this article, the aim is to bridge the gap in the international relations (IR) literature on contemporary interventionism between a strand of research mainly focusing on the concepts of intervention, sovereignty and their meanings, and a strand more interested in the particular practices bound up with the phenomenon described as ‘intervention'. This is done by exploring how the literature on the so-called ‘practice-turn' might allow light to be shed on both dimensions. Such an approach might prove fruitful provided attention is paid both to the material and discursive practices of interventionism; both to the transgressive practices constitutive of interventionism and their routinization. Finally, this piece also introduces each of this special section's contributions by showing how they illustrate and expand on the different problématiques here outlined.  相似文献   
10.
Ongoing human–long-tailed macaque (Macaca fascicularis) conflicts in Bukit Timah Nature Reserve, Singapore, have seen native macaques significantly affected, as residential development encroaches into animals' habitat, destroying important wildlife corridors. The search for a more humane treatment of these transgressive animals can be seen as an attempt to extend and include non-human animals within humanistic notions of ethics and care, in the process destabilizing the assumed divide between human/animal. Yet, a feasible solution is difficult to reach as National Parks Board (NParks), the state agency overseeing the conservation of reserves and wildlife, has to negotiate constantly between their goal of maintaining biodiversity and appeasing the complaining residents. The paper seek to understand urban–wilderness conflicts between human–macaque, showing that the divide between tamed/wild is multi-sited, ambiguous and constantly shifting. In this regard, we are especially interested in the role of intermediaries in initiating actions to ‘make discursive as well as material space’ for macaques in the reserve. Intermediaries, here referring to NParks and animal activists, are actors who do not reside near the reserve thus having no frequent encounters with wildlife, yet are enrolled as mitigators during instances of human–animal conflicts.  相似文献   
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