Nature,Capital and Neighborhoods: “Dispossession without Accumulation”?

Abstract: The ongoing economic crisis, which originated in the USA and has since spread rapidly to capital markets worldwide, is massive, complex, and many times contradictory. One could say the same for responses to the crisis as governments, firms and multi‐national institutions struggle to grasp the full magnitude of the event. This article interrogates the key commodities involved—land, labor and money—and the always‐uneasy relations between spaces of social reproduction and capital. Such ambivalence is critical to understanding how new economic realities are formed in light of retreating neoliberalism as markets become destabilized. The analysis provided suggests the commodities involved in the housing crisis are the basis for a countermovement against dispossession.     

Overpressure and petroleum generation and accumulation in the Dongying Depression of the Bohaiwan Basin, China

The occurrence of abnormally high formation pressures in the Dongying Depression of the Bohaiwan Basin, a prolific oil‐producing province in China, is controlled by rapid sedimentation and the distribution of centres of active petroleum generation. Abnormally high pressures, demonstrated by drill stem test (DST) and well log data, occur in the third and fourth members (Es3 and Es4) of the Eocene Shahejie Formation. Pressure gradients in these members commonly fall in the range 0.012–0.016 MPa m^?1, although gradients as high as 0.018 MPa m^?1 have been encountered. The zone of strongest overpressuring coincides with the areas in the central basin where the principal lacustrine source rocks, which comprise types I and II kerogen and have a high organic carbon content (>2%, ranging to 7.3%), are actively generating petroleum at the present day. The magnitude of overpressuring is related not only to the burial depth of the source rocks, but to the types of kerogen they contain. In the central basin, the pressure gradient within submember Es32, which contains predominantly type II kerogen, falls in the range 0.013–0.014 MPa m^?1. Larger gradients of 0.014–0.016 MPa m^?1 occur in submember Es33 and member Es4, which contain mixed type I and II kerogen. Numerical modelling indicates that, although overpressures are influenced by hydrocarbon generation, the primary control on overpressure in the basin comes from the effects of sediment compaction disequilibrium. A large number of oil pools have been discovered in the domes and faulted anticlines of the normally pressured strata overlying the overpressured sediments; the results of this study suggest that isolated sandstone reservoirs within the overpressured zone itself offer significant hydrocarbon potential.     

商周印纹硬陶与原始瓷器研究

本文讨论了中国古代高温釉器物的起源、基本特征、产地 ,以及陶瓷器族群不同种类的界定与命名等问题。作者认为 ,陶器和瓷器从商周时期开始形成两个不同的发展序列 ,二者各自发展 ,互有影响 ,且时代越晚 ,其关系越疏远。二者的联结点是特殊的陶器———印纹硬陶。     

Wooly mammoth mass accumulation next to the Paleolithic Yana RHS site,Arctic Siberia: its geology,age, and relation to past human activity

In 2001, the Yana RHS archaeological site was discovered in the lower Yana river valley, Arctic Siberia. Its radiocarbon age is about 28 000 BP. While enormous amount of Pleistocene mammal bones was excavated from the site, the mammoth bones occurred at an unexpectedly low frequency. That was interpreted as an indication of the limited role of mammoths in the subsistence economy of the Pleistocene Yana people. In 2008, next to the excavation local ivory miners opened a mass accumulation of mammoth accompanied by the artifacts. About one thousand mammoth bones from at least 26 individuals, and few wooly rhinoceros, bison, horse, reindeer, and bear bones have been unearthed there. Stratigraphy and radiocarbon dating provide evidence for cultural layer of Yana RHS and the mass accumulation of mammoth to be coeval. The geology and taphonomy of Yana mass accumulation of mammoth indicate its anthropogenic nature. Discovery of the anthropogenic mass accumulation of mammoth next to the Yana site suggests a greater role of mammoth in the subsistence practices of the Pleistocene Yana people than previously thought.     

Carbon accumulation and C/N ratios of peat bogs in North‐West Scotland

Three different Scottish peat bogs were sampled, dated and analysed for carbon (C) and nitrogen (N) concentrations. The mean long‐term apparent rate of C accumulation (LARCA) for the three bogs is 213 g C m^～2 yr^‐1’ over the past eight to nine thousand years, comparable to estimates from other parts of the world with similar climate conditions. Within the catotelm portion of peat sequences, the LARCA is variable, ranging from 4.1 to 72.5 g C m^～2 yr^～1. Rates were highest in the early Holocene, in peat rich in woody fragments, and lowest in the mid‐Holocene during drier periods, followed by increased rates during the late Holocene. Analysis of C/N ratios shows a significant positive correlation with peat humification. This may be because past changes in bog wetness affected the C/N ratios of newly forming peat by altering rates of N mineralisation and loss before incorporation of peat into the catotelm.