Sentence examples for marine value from inspiring English sources

The strontium isotope signature of Sikou dolomites and calcite ranges from 0.710210 to 0.710844 and is significantly higher than the Eocene marine value, but this isotope signature is similar to the surrounding Cambrian and Ordovician carbonate bedrock.

The 87Sr/86Sr ratio of the lime mudstones and dolomitized mudstones ranges from 0.7107 to 0.7113 and is significantly higher than the Eocene marine value, but is similar to the surrounding Cambrian and Ordovician carbonate bedrock, which ranges from 0.7096 to 0.7140 (Fig. 8).

In addition, many freshwater endmembers are measurably distinct from the globally homogenous marine value of 0.7092 [23].

The mean measured and corrected 87Sr/86Sr ratio (normalized to 86Sr/88Sr = 0.1194) was 0.70916±0.00006 (SD), within one standard deviation of the global marine value (0.70918).

Mike's series got the annual land and marine values while the other two got April-Sept for NH land N of 20N.

Including marine values influenced terrestrial reserve designs most when terrestrial habitat targets were low and little or none of the target was represented in pre-existing protected areas.

Our results suggest that including marine values in the planning process will influence marbled murrelet terrestrial reserve designs most where substantial terrestrial nesting habitat still exists, where new reserves are relatively unconstrained by pre-existing reserves, or when conservation resources only allow the protection of a small fraction of available habitat.

The isotope values of bulk limestone samples indicate that the carbon and oxygen ratios of the Sikou carbonates differ significantly from the Eocene marine values, which range from δ13C ≈ 1.5 2 ‰ VPDB and δ18O ≈ −1 to 0 ‰ VPDB (Veizer et al. 1999).

Open image in new window Fig. 8 87Sr/86Sr isotope plot of different samples, I is from the samples in the Sikou Sag; II and III represent the surrounding Cambrian and Ordovician carbonate bedrock (Liu et al. 2007); IV represents the Eocene marine values (Veizer et al. 1999).

In this case, Sr/Ba ratios indicated gradual movement across salinity gradients while 87Sr/86Sr ratios remained steady at marine values.

The database, created for Biosecurity New Zealand to assist in the effective management of the New Zealand coastline, comprises 14 attributes of marine environmental value derived from 200 unique layers of environmental information ranging from species occurrences and diversity indices to marine-mammal breeding areas and habitat distribution.