from the South China Sea and a branch of the Kuroshio south of Taiwan reach only the southern part of the Taiwan Strait and that in no way do they flow up freely through the northern part of the Taiwan Strait. This is a clear sign that in winter most of the TWC must originate in ...
The oyster shells used in the present study originate from collections of the Shanghai Natural History Museum and are now permanently stored in the collections of Nanjing University (School of Earth Sciences and Engineering). They have a mid-Holocene age, were found in the central Yangtze River ...
The observed distribution of 未 18 O supports the hypothesis that water masses inside the ring originate from the Kuroshio. Distributions of chemical tracers reveal a strong vertical disturbance of the isolines at the edge of ring 94S, where it approaches the shelf. This phenomenon may play an ...
The adjustment of currents may originate from anomalous NAFW in remote regions. Therefore the temperature response lags the NAFW forcing longer (17–18 months, Table 2) with a correlation coefficient of 0.25–0.47. As a result, the temperature response in the surface layer lags the salinity ...
For the WW coral, these algal biomarkers originate from their symbiotic zooxanthellae40,41, as the zooxanthellae Scientific Reports | 6:18715 | DOI: 10.1038/srep18715 4 www.nature.com/scientificreports/ Figure 4. Distribution of coral mucus C in sponge phospholipid fatty acids (PLFAs). ...
Interpretation: Intraclastic carbonate breccias within the uppermost part of the Gipshuken Formation originate from the prolonged emersion of the platform strata during periods of low sea level. Subjected to a supratidal sabkha environment, already lithified peritidal platform deposits developed into carb...
In Fig. 4b, besides the weak ZPLs, we can observe several intense emission lines ranging from 630 to 637 nm, which originate from the electric dipole vibronic transitions induced by lattice vibrations with odd-parity. Consistently, at 3 K, phonon side- bands arising from the upper sublevel ...