Jotería Listening

This essay is a mapping of Latinx queer listening practices and spaces, such as bars and restaurants, as forms of resistance to gentrification in the Silver Lake neighborhood of Los Angeles. Using a framework called “joteria listening,” and following the route of a performance event and ritual called LA Queer Posada in 2011, the author charts a sonic trail composed of sounds, songs, and memories of places and people in Silver Lake displaced by gentrification and historical erasure. Drawing from sound studies, performance studies and joteria studies, and using oral histories, interviews, archival sources, and ethnography, this essay offers innovative ways to think of queer Latinx sound and space as it adds layers to the palimpsestic map of Silver Lake and beyond. While listening to urban hauntings, sounds of loss, celebration and resistance, it offers new ways of remembering, performing and imagining community, futurity, and a more just world.

Minority shareholder treatment surrounding the Dell MBO

PurposeThis paper is a clinical examination of the October 2013 Management Buyout of Dell Inc. by founder Michael Dell and Silver Lake Partners for a total consideration of $13.88 per share. The proposed transaction was targeted by shareholders unhappy with the deal price and voting framework. Various shareholders went on to file an appraisal suit. Examining these events yields insights into shareholder rights issues in a major transaction.Design/methodology/approachThe paper examines events surrounding the acquisition including the negotiation process, go-shop period, shareholder activist demands for a higher price, shareholder voting and the subsequent appraisal trial and appeal.FindingsDespite suggesting Dell's board fulfilled its fiduciary duties, Delaware Vice Chancellor Travis Laster awarded petitioning shareholders $17.62 per share, a 27% premium to the final deal consideration. This article draws on Laster's decision and research examining topics raised by the surrounding events to argue minority shareholder interests were not sufficiently protected.Research limitations/implicationsThe Dell transaction represents only one data point. Moreover, Vice Chancellor Laster's decision was reversed on appeal.Originality/valueNevertheless, the paper discusses the nuances surrounding many issues of interest to practitioners involving large going private transactions. It could also be used to illustrate many “real world” perspectives in an advanced corporate finance or mergers and acquisitions class.

Holocene subalpine forest-parkland dynamics in Big Cottonwood Canyon, Wasatch Mountains, Utah, USA

Understanding long-term responses of subalpine forest-parklands to Holocene climate variability in local context is critical for better managing those ecosystems under future climate change. Available records suggest that western North American subalpine forest-parkland ecosystems responded to Holocene climate in various ways at different places. Here we present a Holocene record of upper montane forest-parkland dynamics from Silver Lake in Big Cottonwood Canyon, Wasatch Range, on the Great Basin’s eastern margin. Our results show that at the end of the Younger Dryas, Silver Lake was surrounded by open Pinus/Picea parkland mixed with Artemisia subalpine steppe. By ~9.0 cal ka BP Picea began to expand in response to early Holocene summer warming and enhanced winter moisture. Picea-dominated forests prevailed from ~8.0 to 5.0 cal ka BP, after which time a more open Picea parkland developed. By ~3.5 cal ka BP Pinus increased under cooling conditions, and Picea gradually rebounded to form the mixed conifer forest present today. The Silver Lake long-term record of moderate shifts within an upper montane ecosystem is consistent with other regional sites in the timing of major vegetation changes reflecting large-scale climatic forcings, but distinct in response to local factors including the importance of enhanced lake-effect snowpack and the absence of competing lower montane Pinus. These local factors may help account for the long-term stability of Picea-dominated forests in the area.

Vegetation Changes Associated with the Younger Dryas from the Sediments of Silver Lake, Summit County, Ohio, USA

As the climate was warming during the last deglaciation, a millennium-long return to near-glacial conditions—called the Younger Dryas (YD) stadial—occurred about 12.9 to 11.7 ka ago. Prior studies have characterized the vegetation and climatic impacts of the YD stadial in the US upper Midwest from a network of fossil pollen records. The goal of this study was to locate the pronounced rise in organic matter and Pinus (pine) pollen—associated with the latter part of the YD event—in a sediment core from Silver Lake, a kettle lake in Summit County, Ohio. Based upon radiocarbon dating of the Silver Lake sediment core, an increase in sediment organic matter at 1,070 cm (35.1 ft) core depth dates to 12,130 calibrated years (cal yr) BP within the latter part of the YD stadial. A pollen study spanning the change in organic matter displays a gradual decline in Picea (spruce) pollen as well as a pronounced increase in Pinus pollen, similar to published records of the latter part of the YD event. Thus, the Silver Lake pollen record adds a new site to the network of fossil pollen sites, and further refines the vegetation changes within the Allegheny Plateau of Ohio that occurred during the latter part of the YD event. Furthermore, identifying the pronounced rise in Pinus pollen allows for biostratigraphic correlation between the Silver Lake record and another local dated pollen record. This biocorrelation adds further support to the Silver Lake radiometric age model.

Interpreting basal sediments and plant fossils in kettle lakes: insights from Silver Lake, Michigan, USA

We report on pollen, plant macrofossils, and associated lithostratigraphy of a sediment core extracted from the base of Silver Lake, a kettle lake in northern Lower Michigan, USA, which reveal a complex deglacial scenario for ice block melting and lake formation, and subsequent plant colonization. Complementary multivariate statistical and squared chord distance analyses of the pollen data support these interpretations. The basal radiocarbon age from the core (17 540 cal years BP) is rejected as being anomalously old, based on biostratigraphic anomalies in the core and the date’s incongruity with respect to the accepted regional deglaciation chronology. We reason that this erroneous age estimate resulted from the redeposition of middle-Wisconsin-age fossils by the ice sheet, mixed with the remains of plants that existed as the kettle lake formed at ca. 10 940 cal years BP by ice block ablation. Thereafter, the kettle lake became a reliable repository of Holocene-age fossils, documenting a mature boreal forest that existed until 10 640 cal years BP, followed by a pine-dominated mixed forest, an early variant of the mixed conifer–hardwood forest that persists to the present day. Our study demonstrates that researchers investigating kettle lakes, a common depositional archive for plant fossils in deglaciated landscapes, should exercise caution in interpreting the basal (Late Pleistocene/early Holocene-age) part of lake sediment cores.

Pesona Silver Lake Sebagai Obyek Wisata Di Pattaya Thailand

Makalah ini merupakan hasil laporan Foreign Case Study untuk syarat publikasi ilmiah di Sekolah Tinggi Pariwasata Ambarrukmo Yogyakarta dengan judul Pesona Silver Lake Sebagai Obyek Wisata Di Pattaya Thailand.