Burning books and burying scholars: on the policies of the short-lived Qin Dynasty in ancient China (221-207 BC)

In 221 BC, the battle-hardened warriors of the Qin state, the western frontier state and the most aggressive of the Warring States, subjugated the last of its rival states, thus establishing the Qin dynasty, with itscapital in Xianyang, near the modern Xi’an. The Qin dynasty is customarily regarded by Chinese and Western scholars as the beginning of a new age – the Chinese empire – that lasted until 1911 AD. The dynasty lasted only fifteen years. This study examines the main policies of the Qin dynasty and seeks to address the question what brought the quick downfall of the Qin rule. This paper takes the cultural and political contexts carefully into consideration, and argues that the Qin annexation of its rival states might be better understood as an end of an old era as much as a beginning of a new epoch.

Recovery pattern of brachiopods after the Permian-Triassic crisis in South China

In South China, the Changhsingian brachiopods are extraordinarily abundant and diverse, comprising 468 species in 144 genera. However, approximately 91% of brachiopod species were eliminated during the Permian-Triassic (P-Tr) mass extinction event. Brachiopods in the aftermath of the P-Tr mass extinction were extremely rare, with only one opportunistic taxon, Lingulida, occasionally found in the Griesbachian and Smithian at a high abundance. Species-diversity of articulated brachiopods in the early Griesbachian, late Griesbachian, Dienerian, and Smithian are 35, 3, 2, and 0, respectively. Although a few of Mesozoic-type species occurred in the Griesbachian, Dienerian and Smithian, a marked diversification of brachiopods occurred in the Spathian and early Anisian and was characterised by 9 and 17 Mesozoic-type species, respectively. The diversification of brachiopods in the Spathian and early Anisian coincides with the contemporaneous expansion of the refuge zone, suggesting that the improvement of marine environmental conditions (e.g., lethally hot temperature and anoxic seawater) played a key role in brachiopod recovery after the P-Tr mass extinction.

An explanation of capital structure of China's listed property firms

Purpose– The purpose of this paper is to investigate the determinants of the capital structure of listed property firms in China.Design/methodology/approach– The study is based on quantitative methods such as dynamic panel data models and a panel data set containing financial and accounting data for all listed property companies from 2006 to 2010 in China.Findings– The findings confirm that the state-own shares, the fixed asset values, the total size of assets and profitability have a positive and significant impact on the leverage ratio of listed property firms in China. The negative impact of the tax shields and the currency ratio, and significant impact of state-own shares on capital structure cannot be explained by existing capital structure theory but the unique property market regulation environment and market conditions in China.Research limitations/implications– The findings confirm the applicability of trade-off theory (except for the correlation between leverage and the tax shield) on property companies in China. They also highlight the importance of government policies and special market conditions in explaining the financing behaviour of property companies in transaction countries like China.Practical implications– Complimentary policies should be established along with property market restriction policies to offset their unequal negative effect on property companies with less state-owned shares. Furthermore, government should invest efforts to eliminate the discrimination credit treatment of banks against property companies with non-existent or few state-owned shares.Originality/value– The special financial behaviour of China's property firms and the unique financial and property market conditions highlight the necessity of researching the capital structure of listed property firms in China. However, most of the existing literature focuses on the company financial behaviour in developed countries, and very few studies have been done concerning property firms’ financing behaviour in emerging economies such as China, and this research prospects to fill this blank.

Health-related quality of life and willingness to pay per quality-adjusted life-Year threshold—A study in patients with epilepsy in China

Objectives
To assess the health-related quality of life (HRQOL) and willingness to pay (WTP) per quality-adjusted life-year (QALY) amount of patients with epilepsy in China.
Methods
Adults with epilepsy and a healthy control were recruited in two tertiary hospitals in China. Participants completed two indirect utility elicitation instruments (Quality of Well-being Scale-self administered version and EuroQol five-dimensional questionnaire) and a WTP questionnaire. Correlations between sociodemographic or epilepsy-specific variables (age of epilepsy onset, duration of epilepsy, seizure types, types of antiepileptic drug treatment, etc.) and HRQOL or WTP/QALY were assessed to identify the candidate predictor. Multiple linear regression models were adopted to investigate the predictive performances of identified candidate predictors. Data analyses were performed on SPSS 20.0 (SPSS, Inc., Chicago, IL).
Results
For utilities of both the Quality of Well-being Scale-self administered version and the EuroQol five-dimensional questionnaire, patients with epilepsy had statistically lower values than did the control group (P < 0.0001). In terms of the WTP/month, the percentage of WTP accounting for the monthly income and the WTP/QALY values from the epilepsy group were substantially higher than those from the control group (P < 0.0001).
View the MathML sourceWTP/QALY=12×WTPMonth1−Utility(CurrentHealth)
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The multiple linear regression model identified working status (P = 0.05), seizure types (P = 0.022), income (P = 0.006), and self-rating health state (P < 0.05) as predictors of HRQOL while income (P = 0.000) and self-rating health state (P < 0.05) statistically contributed to the variations in WTP/QALY value for the epilepsy group.
Conclusions
Patients with epilepsy had substantially lower HRQOL than did the healthy population.

Early Triassic disaster and opportunistic foraminifers in South China

Survival and recovery are important dynamic processes of biotic evolution during major geological transitions. Disaster and opportunistic taxa are two significant groups that dominate the ecosystem in the aftermath of mass extinction events. Disaster taxa appear immediately after such crises whilst opportunists pre-date the crisis but also bloom in the aftermath. This paper documents three disaster foraminiferal species and seven opportunistic foraminiferal species from Lower Triassic successions of South China. They are characterized by extreme high abundance and low diversity and occurred occasionally in Griesbachian, Smithian and Spathian strata. The characteristics (small size, simple morphology) and stratigraphic ranges of these groups suggest that r-selection is a commonly used strategy for survivors to cope with either harsh post-extinction conditions and/or environments lacking incumbents.

Upper lower triassic stromatolite from Anhui, South China: geobiologic features and paleoenvironmental implications

Widespread stromatolites and other microbialite deposits characterize Lower Triassic marine successions worldwide. This study documents a stromatolite deposit, 1.1. m thick, from the upper Spathian (Lower Triassic) of the Susong area, South China. The stromatolite comprises distinct laminated domes in the basal part and columns at the upper part. Dark laminae are loosely spaced and interlayered with thicker light colored laminae. Diffusive dark colored laminae are composed of peloidal micrite that grade locally into microclotted structures, and yield copies of bacteria clump-like and coccoid-like spheroid aggregates. The former are characterized by cloudy, micrite nuclei rimmed by coarse-grained, euhedral sparry calcite crystals, while the latter are comprised of solid calcite crystal nuclei coated with rather thin micrite envelopes. The cloudy, micrite nuclei resemble bacteria clump-like structures observed in present-day travertine. Both the coccoid-like spheroids and bacteria clump-like structures are surrounded by coarse-grained euhedral calcite crystals, suggesting a similar accretion mechanism. Both spherical structures therefore could be crucial in the accretion of the Susong stromatolite. The laminated/microclotted structures are interpreted as the result of variation in timing of lithification relative to the timing of the decay of microbes. Micro-analysis also unravels the common occurrence of authigenic micro-quartz crystals in association with Fe-bearing illite clay minerals in the stromatolite columns. Their coalescing nature with each other, together with the associated pyrite grains, strongly support the formation of micro-quartz crystals from microbial reduction of an Fe-bearing smectite precursor by sulfate reducing bacteria. A comparison of the Susong stromatolite with its counterparts from the upper Lower Triassic strata in Dajiang, South China reveals many similarities in stromatolite microstructures, suggesting that a harsh, euxinic-anoxic environment resulting in the bloom of sulfate reducing bacteria most likely extended into the latest Spathian in South China.

Taphonomy and palaeobiology of early Middle Triassic coprolites from the Luoping biota, southwest China: implications for reconstruction of fossil food webs

Abundant, exceptionally preserved coprolites are documented from the Luoping biota (Anisian, Middle Triassic) of Yunnan Province, southwest China. These coprolites can be categorized into fourmorphological types: A) bead to ribbon-shaped, B) short to long cylindrical-shaped, C) flattened, disk-like, and D) segmented faeces. Detailed multi-disciplinary studies reveal that coprolite type A was likely produced by invertebrate animals,while coprolite types B to D could be faeces generated by carnivorous fishes or marine reptiles, perhaps from different taxonomicgroups. When compared with coprolites reported from the Lower Triassic, the Luoping forms indicate more complicated predation-prey food web networks. These evidences, combined with body fossil discoveries fromLuoping, suggest the emergence of complex trophic ecosystems in the Anisian,marking the full biotic recovery following the Permian–Triassic Mass Extinction.