No evidence for an afrotherian-like delayed dental eruption in South American notoungulates

The fossil South American ungulates are of great interest relative to the new phylogenetic framework elaborated for living placental mammals. In particular, studies on these endemic taxa can allow for testing congruence between southern placental phylogeny and plate tectonics, beyond what has already been suggested in the Atlantogenata hypothesis based on extant afrotherians and xenarthrans. The presence of delayed dental eruption relative to skull growth is one feature characterizing the extant afrotherians and possibly the xenarthrans. Late dental eruption has been mentioned previously in South American notoungulates, thus suggesting possible resemblance with afrotherians and perhaps xenarthrans. We provide here a detailed study of the dental eruption pattern relative to the skull growth in the notoungulates. In contrast to previous statements, our results demonstrate that there is currently no evidence for an afrotherian-like delayed dental eruption in this group. For now, the inferred absence of a delayed dental eruption in notoungulates does not support atlantogenatan/afrotherian affinities for the Notoungulata, but other atlantogenatan/afrotherian characteristics remain to be explored in more detail in this group and other South American ungulates.     

A previously unrecognized group of Middle Jurassic triconodontan mammals from Central Asia

Ferganodon narynensis gen. et sp. nov. is represented by a lower molariform tooth from the Middle Jurassic (Callovian) Balabansai Svita in Kyrgyzstan. The new genus is allied with Klamelia zhaopengi Chow and Rich 1984 from the Middle Jurassic Shishugou Formation in Xinjiang, northwest China to the new family Klameliidae based on parallelogram-shaped lower molariforms, imbricating rather than interlocking of cusps e-d-f, by a peculiar distolabial cingulid cusp, and by vertical folding of the enamel on the labial crown side. The new family Klameliidae fam. nov. is most similar to Gobiconodontidae by the structure of the molariform teeth and represents a previously unrecognized radiation of eutriconodontan mammals possibly endemic to Central Asia.     

Ordering phenomena in quasi-one-dimensional organic conductors

Low-dimensional organic conductors could establish themselves as model systems for the investigation of the physics in reduced dimensions. In the metallic state of a one-dimensional solid, Fermi liquid theory breaks down and spin and charge degrees of freedom become separated. But the metallic phase is not stable in one dimension: as the temperature is reduced, the electronic charge and spin tend to arrange themselves in an ordered fashion due to strong correlations. The competition of the different interactions is responsible for which broken-symmetry ground state is eventually realized in a specific compound and which drives the system toward an insulating state. Here, we review the various ordering phenomena and how they can be identified by optic and magnetic measurements. While the final results might look very similar in the case of a charge density wave and a charge-ordered metal, for instance, the physical cause is completely different. When density waves form, a gap opens in the density of states at the Fermi energy due to nesting of the one-dimension Fermi surface sheets. When a one-dimensional metal becomes a charge-ordered Mott insulator, on the other hand, the short-range Coulomb repulsion localizes the charge on the lattice sites and even causes certain charge patterns. We try to point out the similarities and conceptional differences of these phenomena and give an example for each of them. Particular emphasis will be put on collective phenomena that are inherently present as soon as ordering breaks the symmetry of the system.     

Economics of dairy waste use as fertilizer in central Texas

Dairy manure is an unavoidable natural, but negative, byproduct of milk production. Its nitrogen, phosphate, and potash contents represent a potential substitute for commercial fertilizers on field crops. In the absence of subsidies, manure transportation and land application costs limit its utilization as a substitute for chemical fertilizer. The results from a study of the economics of manure use in Central Texas suggest that, at the current costs for loading, hauling, and spreading, dairy manure cannot be economically transported from surplus to deficit areas within the study area. The estimated breakeven transport distance for manure application to four crops varied from 28 to 41 km; however, the distances between manure-surplus and manure-deficit counties in the study region varied from 40 to 90 km. An analysis of potential subsidies paid by the government or dairy farmers showed that the breakeven distance could increase by up to 30 km. A decrease in the assumed moisture content of the manure from 50% to 40% is shown to increase the breakeven distance by 10 km. The study suggests that dairy manure loading, transportation, and land application, with appropriate subsidies or reductions in moisture content, has the potential to be profitably substituted for chemical fertilizers.     

Nitrogen oxide and methane emissions under varying tillage and fertilizer management

Comprehensive assessment of the total greenhouse gas (GHG) budget of reduced tillage agricultural systems must consider emissions of nitrous oxide (N2O) and methane (CH4), each of which have higher global warming potentials than carbon dioxide (CO2). Tillage intensity may also impact nitric oxide (NO) emissions, which can have various environmental and agronomic impacts. In 2003 and 2004, we used chambers to measure N2O, CH4, and NO fluxes from plots that had been managed under differing tillage intensity since 1991. The effect of tillage on non-CO2 GHG emissions varied, in both magnitude and direction, depending on fertilizer practices. Emissions of N2O following broadcast urea (BU) application were higher under no till (NT) and conservation tillage (CsT) compared to conventional tillage (CT). In contrast, following anhydrous ammonia (AA) injection, N2O emissions were higher under CT and CsT compared to NT. Emissions following surface urea ammonium nitrate (UAN) application did not vary with tillage. Total growing season non-CO2 GHG emissions were equivalent to CO2 emissions of 0.15 to 1.9 Mg CO2 ha(-1) yr(-1) or 0.04 to 0.53 Mg soil-C ha(-1) yr(-1). Emissions of N2O from AA-amended plots were two to four times greater than UAN- and BU-amended plots. Total NO + N2O losses in the UAN treatment were approximately 50% lower than AA and BU. This study demonstrates that N2O emissions can represent a substantial component of the total GHG budget of reduced tillage systems, and that interactions between fertilizer and tillage practices can be important in controlling non-CO2 GHG emissions.     

Extinction may not be forever

Here we review the phenomenon of ecomorph evolution and the hypothesis of iterative climatic cycles. Although a widely known phenomenon, convergent evolution has been underappreciated in both its scope and commonality. The power of natural selection to override genealogy to create similar morphologies (even among distantly related organisms) supports classical Darwinian evolution. That this occurs repeatedly in stratigraphically closely spaced intervals is one of the most striking features of Earth history. Periodic extinctions followed by re-evolution of adaptive types (ecomorphs) are not isolated occurrences but are embedded within complex ecological systems that evolve, become extinct, and repeat themselves in temporal synchrony. These complexes of radiation and extinction bundle the biostratigraphic record and provide the basis for a global stratigraphy. At this scale, climatic change is the only mechanism adequate to explain the observed record of repeating faunas and floras. Understanding of the underlying causes may lead to predictive theories of global biostratigraphy, evolutionary processes, and climatic change.