A thick (ca. 40 m) sequence of coastal eolian sediments occurs on a narrow peninsula on the eastern end of the island of Madeira, located in the Eastern Atlantic at 33°N latitude. The sediments consist of black volcanic sands (with or without bioclasts) as well as clay units up to 2 m thick. A series of inceptisols (Eutrochrepts) and one alfisol (a Hapludalf) are developed in these sediments. Land snail shells and secondary carbonates, in the form of well-developed rhizoliths, calcretes, fissure-fills, and soil nodules, are present in abundance. The chronology of the sequence was determined by 14C and U---Th analyses of land snail shells and secondary carbonates and amino acid epimerization analysis of land snail shells. All sediments, including the clay units, are originally of eolian origin, derived from the beach to the south of the deposit, but some have been redeposited by colluviation. Temporal variation in the lithology of the sediments relates to variations in sea-level, with black sands being deposited during lower sea level stands and clays at the lowest. It is suggested that fine marine sediments, exposed during low sea-level stands, may also be the dominant source of silty or clayey units in other coastal eolian deposits in the subtropical Atlantic and Mediterranean.
The sequence spans from 200,000–300,000 years ago up to the 20th century. Sedimentation was discontinuous and often rapid; erosional hiatuses are present. During the Holocene, eolian sands started accumulating at 8200 yr B.P. during a transgressive phase and stopped at 4500 yr B.P. as sea level approached its present height. Colluviation increased dramatically following the first human settlement of the island in the 15th century and continued up to the 20th century, as dated by amino acid epimerization analysis of land snails. Earlier periods of colluviation were identified from the age distribution of land snail shells redeposited in younger colluvium.
Paleoenvironmental reconstruction was based mainly on soil and sediment features (including rhizolith morphology) and land snail faunas but also on stable isotope variations (13C, 18O) in land snails and secondary carbonates, pollen (generally not well preserved), and phytoliths. Most of the portion of the Middle Pleistocene represented in the sequence was characterized by moderately dry conditions, in comparison to the late Pleistocene and Holocene. During the last interglacial, relatively wet conditions occurred, wetter than during the Holocene interglacial. Moderately moist conditions were present during the accumulation of the thick unit dating to ca. 80,000 yr B.P. As sea level fell subsequent to this period, conditions appear to have become drier. Starting ca. 50,000–55,000 yr B.P., conditions were especially wet, but prior to the last glacial maximum, markedly arid conditions ensued. Toward the end of the last glacial, wet conditions returned and produced the best-developed soil preserved in the sequence. Moderately moist conditions occurred during the early to middle Holocene but apparently become slightly drier after 4500 yr B.P. The impact of human settlement can be seen in the loss of woody vegetation and enhanced gullying and colluviation during the last ca. 500 years. 相似文献
In trees and other woody perennial plants, short days (SDs) typically induce growth cessation, the initiation of cold acclimation, the formation of a terminal bud and bud dormancy. Phytochrome control of SD-induced bud set was investigated in two northern clones of black cottonwood (Populus trichocarpa Torr. & Gray) by using night breaks with red light (R) and far-red light (FR). For both clones (BC-1 and BC-2), SD-induced bud set was prevented when R night breaks as short as 2 min were given in the middle of the night. When night breaks with 2 min of R were immediately followed by 2 min of FR, substantial reversibility of bud set was observed for BC-1 but not for BC-2. By comparing the effects of the R night breaks on bud set and the length of specific internodes, we determined that the R night breaks influenced internode elongation in two opposing ways. First, the addition of a R night break to the SD treatment prevented the cessation of internode elongation that is associated with bud set. Those internodes that would not have elongated under SDs (and would have been found within the terminal bud) elongated in the R treatment. Second, the R night breaks decreased internode length relative to the long-day (LD) control. In contrast to the clonal differences in reversibility that we observed for bud set, the decrease in internode length (i.e. the second effect of R) was R/FR reversible in both clones. Based on these results, we conclude that internode elongation is influenced by two distinct types of phytochrome-mediated response. The first response is a typical response to photpperiod, whereas the second response is a typical “end-of-day” response to light quality. Our results demonstrate that SD-induced bud set in black cottonwood is controlled by phytochrome but that clonal differences have an important influence on the R/FR reversibility of this response. The availability of an experimental system in which SD-induced bud set is R/FR reversible will be valuable for studying the physiological genetics of photoperiodism in trees. 相似文献
Amplification of thebar gene usingTaq DNA polymerase in PCR is often not successful, possibly due tobar's high GC content. We describe a PCR protocol in which reliable amplification at a sensitivity of one gene copy per genome
(in this study, barley) present in the reaction was achieved using a novel pair of primers and Expandtm High Fidelity DNA polymerase mix (Boehringer Mannheim). This method should allow for rapid screening of plants putatively
transformed withbar. 相似文献
Root nodule bacteria and Escherichia coli show an adaptive acid tolerance response when grown under mildly acidic conditions. This is defined in terms of the rate of cell death upon exposure to acid shock at pH 3.0 and expressed in terms of a decimal reduction time, D. The D values varied with the strain and the pH of the culture medium. Early exponential phase cells of three strains of Rhizobium leguminosarum (WU95, 3001 and WSM710) had D values of 1, 6 and 5 min respectively when grown at pH 7.0; and D values of 5, 20 and 12 min respectively when grown at pH 5.0. Exponential phase cells of Rhizobium tropici UMR1899, Bradyrhizobium japonicum USDA110 and peanut Bradyrhizobium sp. NC92 were more tolerant with D values of 31, 35 and 42 min when grown at pH 7.0; and 56, 86 and 68 min when grown at pH 5.0. Cells of E. coli UB1301 in early exponential phase at pH 7.0 had a D value of 16 min, whereas at pH 5.0 it was 76 min. Stationary phase cells of R. leguminosarum and E. coli were more tolerant (D values usually 2 to 5-fold higher) than those in exponential phase. Cells of R. leguminosarum bv. trifolii 3001 or E. coli UB1301 transferred from cultures at pH. 7.0 to medium at pH 5.0 grew immediately and induced the acid tolerance response within one generation. This was prevented by the addition of chloramphenicol. Acidadapted cells of Rhizobium leguminosarum bv. trifolii WU95 and 3001; or E. coli UB1301, M3503 and M3504 were as sensitive to UV light as those grown at neutral pH. 相似文献
During studies on the fucosylation of endogenous proteins inparental (Pro5) and N-acetyl-D-glucosamine (GlcNAc) transferaseI-deficient (Lec1) Chinese hamster ovary (CHO) cells, we observedthat Lec1 cells incorporate 相似文献
The Triassic marine reptiles at the base of the extinct Order Sauropterygia, traditionally known as nothosaurs, represent an unnatural assemblage of superficially similar forms. The traditional grouping of these animals has generally relied on the flawed basis of “primitive” characteristics whereas two distinct nothosaurian lineages can now be identified through the use of cladistic methodology. The Pachypleurosauria are the most plesiomorphic, but not the earliest, sauropterygians known. The Nothosauriformes include not only ‘nothosaurs’ but also the monophyletic group Plesiosauria and seemingly also the Placodontia. Rigorous coding of characters for the recently described nothosaurian genusSilvestrosaurus allows expansion of the phylogenetic data base for the Sauropterygia. The revised analysis reaffirms recent studies of relationship for the sauropterygians and demonstrates the affinity ofSilvestrosaurus with the Nothosauriformes. The explicit hierarchical classification scheme presented incorporates the hypothesized phylogenetic relationships of these long-misunderstood taxa. The traditional Suborder Nothosauria, now seen to be paraphyletic, must be abandoned. 相似文献
Nucleoside phosphotransferase acting on inosine and deoxyinosine has been partially purified from cultured Chinese hamster lung fibroblasts (V79). The activity is associated with a cytosolic 5′-nucleotidase acting on IMP and deoxyIMP. The transfer of the phosphate group from IMP to inosine catalyzed by this enzyme was activated by ATP and 2,3-bisphosphoglycerate. Inosine, deoxyinosine, guanosine, deoxyguanosine, and the nucleoside analogs 2′,3′-dideoxyinosine and 8-azaguanosine are substrates, while adenosine and deoxyadenosine are not. IMP, deoxyIMP, GMP, and deoxyGMP are the best phosphate donors. The cytosolic 5′-nucleotidase/phosphotransferase substrate, 8-azaguanosine, was found to be very toxic for cultured fibroblasts (LD50 = 0.32 μM). Mutants resistant to either 8-azaguanosine and the correspondent base 8-azaguanine were isolated and characterized. Our results indicated that the 8-azaguanosine-resistant cells were lacking both cytosolic 5′-nucleotidase and hypoxanthine-guanine phosphoribosyltransferase, while 8-azaguanine resistant cells were lacking only the latter enzyme. Despite this observation, both mutants displayed 8-azaguanosine resistance, thus indicating that cytosolic 5′-nucleotidase is not essential for the activation of this nucleoside analog. 相似文献