Abstract. The relative contributions of C3 and C4 plants to vegetation at a given locality may be estimated by means of δ13C of soil organic matter. This approach holds a great potential for paleoecological reconstruction using paleosols. However, two main uncertainties exist, which limits the accuracy of this application. One is δ13C-enrichment as the plant carbon becomes incorporated into soil organic matter. The other is due to environmental influences on δ13C of plants. Two types of data were collected and analyzed with an objective of narrowing the error of paleovegetation reconstruction. First, we investigated δ13C variations of 557 C3 and 136 C4 plants along a precipitation gradient in North China. A strong negative correlation is found between the δ13C value of C3 plants averaged for each site and the annual precipitation with a coefficient of −0.40‰/100mm, while no significant coefficients were found for C4 plants. Second, we measured δ13C of soil organic matters for 14 soil profiles at three sites. The isotopic difference between vegetation and soil organic matter are evaluated to be 1.8‰ for the surface soil and 2.8‰ for the soil at the bottom of soil profiles. We conducted a sample reconstruction of paleovegetation at the central Chinese Loess Plateau during the Holocene and the Last Glacial (LG), and conclude that, without corrections for δ13C-enrichment by decomposition, the C4 abundance would be overestimated. The importance and uncertainties of other corrections are also discussed.
The process of heat regulation is complex and the exact molecular mechanism is not fully understood. To investigate the global gene response to chronic heat exposure, a breast muscle cDNA library and a liver tissue cDNA library from Silkie fowl were constructed and analyzed in bioinformatics. A total of 8,935 nonredundant EST were identified from and used for gene expression analysis. Microarray assay revealed that in breast muscle of broiler chickens (Gallus gallus), 110 genes changed expression levels after 3 wk of cycling heat stress. Ubiquitin B (UBB); ubiquitin C (UBC); tumor necrosis factor receptor-associated factor 3-interacting Jun amino-terminal kinase activating modulator (TRAF3IP3); eukaryotic translation initiation factor 3, subunit 6 (EIF3S6); poly(A) binding protein, cytoplasmic 1 (PABPC1); and F-box only protein 11 (FBXO11) were the only genes that have been reported to be involved in heat regulation; the majority of the other genes were shown to be related for the first time. The finding of new heat-reactive genes [mitogen-activated protein kinase activating protein PM20/PM21; suppressors of cytokine signaling (SOCS) box-containing protein 2 (ASB2); ubiquitin-specific proteinase 45 (USP45); and TRK-fused gene (TFG)] suggests that the mitogen-activated protein kinase pathways as well as the ubiquitin-proteasome pathways and the nuclear factor κB pathways play important roles in heat regulation. This study provides new information on the regulation of heat stress, though the mechanism is far from being understood. Further in-depth research on the newly discovered heat-reactive genes is required to fully understand their molecular functions in thermoregulation.
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