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41.
Siân E. Rees Martin J. Attrill Melanie C. Austen Steven C. Mangi Jo P. Richards Lynda D. Rodwell 《Ocean & Coastal Management》2010,53(3):135-145
A statutory two hundred and six square kilometre ‘closed area’ in Lyme Bay, South West England entered into force on the 11 July 2008 to protect the reef substrate and the associated biodiversity from the impacts of trawling and dredging with heavy demersal fishing gear. This case study provides an example of how the ecosystem approach has been incorporated into decision making for marine nature conservation and shows that despite sound ecological knowledge of a marine area, the current reliance on traditional neo-classical economic valuations for marine spatial planning can obscure other issues pertinent to the ecosystem approach. With the Government seeking win–win scenarios for stakeholders in the designation of Marine Conservation Zones under the Marine and Coastal Access Act, experience of marine spatial planning in Lyme Bay has revealed that a win–win must be a long-term goal based on a thorough evaluation of the environmental, social and economic values of marine biodiversity. 相似文献
42.
Limnology of Two Antarctic Epishelf Lakes and their Potential to Record Periods of Ice Shelf Loss 总被引:1,自引:0,他引:1
James A. Smith Dominic A. Hodgson Michael J. Bentley Elie Verleyen Melanie J. Leng Steven J. Roberts 《Journal of Paleolimnology》2006,35(2):373-394
George VI Ice Shelf is the largest ice shelf on the western side of the Antarctic Peninsula and its northern margin marks
the southern most latitudinal limit of recent ice shelf retreat. As part of a project to reconstruct the long-term (Holocene)
history of George VI Ice Shelf we studied two epishelf lakes impounded by the ice shelf at Ablation Point, on the east coast
of Alexander Island. These lakes, Moutonnée and Ablation, are stratified water bodies with a lower marine layer and an upper
freshwater layer. To determine if their sediment records could be used to detect past changes in the presence or absence of
the ice shelf it was necessary to describe their present-day limnology and sedimentology. We measured water column chemistry
and sampled the water column and sediments of the lakes along vertical and horizontal transects. We analysed these samples
for diatoms, stable isotopes (δ18O, δ2H, δ13CDIC, δ13Corg), geochemistry (TOC, TN, C/N ratios) and physical sedimentology (grain-size). This was supplemented by chemical and biological
reference data from the catchments. Results showed that the water columns of both lakes are nutrient limited and deficient
in phytoplankton. Benthic productivity is low and decreases with depth. Comparison of water column chemistry with an earlier
survey shows a net increase in the thickness of the freshwater layer in Moutonnée Lake between 1973 and 2001, which could
indicate that George VI Ice Shelf has thinned during this period. However, a similar trend was not observed in Ablation Lake
(5 km to the north) and an alternative explanation is that the changes are a seasonal phenomena. Data from the surface sediment
transects identified a number of proxies that respond to the present day stratification of the water column including diatom
species composition, stable isotopes and geochemistry, particularly in Moutonnée Lake. Collectively these data have been used
to develop a conceptual model for determining past ice shelf configuration in epishelf lakes. Specifically, periods of past
ice shelf loss, and the removal of the ice dam, would see the present stratified epishelf lake replaced by a marine embayment.
It is suggested that this change would leave a clear signature in the lake sediment record, notably the deposition of an exclusively
marine biological assemblage, increased ice rafted debris and δ13Corg values that are indicative of marine derived organic matter.
These authors contributed equally to this work 相似文献
43.
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45.
Melanie Louise Inez Witt Stephen Skrabal Robert Kieber Joan Willey 《Journal of Atmospheric Chemistry》2007,58(2):89-109
Significant quenching of fluorescence by Cu in rainwater samples from southeastern North Carolina demonstrates that chromophoric
dissolved organic matter (CDOM) is an effective ligand for Cu in rainwater. A strong inverse correlation between the decrease
in fluorescence upon Cu addition and CDOM abundance suggests the presence of excess binding sites for Cu in high CDOM samples.
Electroanalytical studies indicate that CDOM extracted from C18 cartridges formed Cu complexes with concentrations and conditional stability constants similar to ligands found in ambient
rainwater. When authentic rainwater samples were photolyzed with simulated sunlight both photoproduction and photodestruction
of ligands were observed, suggesting the photochemical response of Cu-complexing ligands in rainwater is the result of two
competing reactions. The rate of CDOM photobleaching was directly related to changes in strong ligands (KCuL ∼ 1015) whereas weaker ligands (KCuL < 1013) were not correlated, suggesting the photolabile CDOM resides in the strong ligand class. A photolysis study comparing filtered
and unfiltered rainwater samples indicated that Cu-complexing ligands adsorbed onto or otherwise associated with particles
are photodegraded much more rapidly than dissolved ligands. Photolysis with UV radiation appears to be most effective at engendering
changes in Cu ligands, however a significant photochemical response was also observed when samples were exposed to photosynthetically
active radiation with wavelengths greater than 400 nm. Results from this study demonstrate that complexation of Cu by CDOM
has important ramifications for controlling both the speciation of the metal and the reactivity of CDOM in rainwater. 相似文献
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48.
Emma Hodgson Stephen T. Grimes Gregory D. Price Meriel E.J. Fitzpatrick Malcolm B. Hart Melanie J. Leng 《Proceedings of the Geologists' Association. Geologists' Association》2011,122(3):460-471
This study demonstrates that the Bunkers Hill borehole, which is located within the Hampshire Basin, contains a carbon isotope excursion (CIE) in the Upnor Formation followed by a positive recovery from another CIE within the overlying Reading Formation. This study has also shown that the CIE in the Upnor Formation predates the Paleocene/Eocene Thermal Maximum (PETM), while the carbon isotope recovery at the base of the Reading Formation is most likely related to it. The positive carbon isotope trend, before a return to more negative values, seen throughout the majority of the Reading Formation can also be seen in coeval deposits in the Jubilee 404T borehole in the London Basin and in the Tienen Formation in the Doel and Kallo boreholes from the Belgium Basin. This indicates that this post-PETM carbon isotope signal may, therefore, be regional if not global in nature. 相似文献
49.
Catherine N. Jex Andy Baker Jonathan M. Eden Warren J. Eastwood Ian J. Fairchild Melanie J. Leng Louise Thomas Hilary J. Sloane 《Quaternary Research》2011,75(3):399-405
A verified instrumental calibration of annually resolved δ18O for a stalagmite from Gümü?hane in northeast Turkey is presented and cross-validated using a ‘leave-one-out’ technique. The amount of late autumn to winter precipitation is negatively correlated with stalagmite δ18O between AD 1938 and 2004. The observed relationship is extrapolated back to ~ AD 1500 leading to the first long winter precipitation reconstruction for this region. Modern day October to January precipitation is linked to pressure fields in Western Russia. Anomalously lower reconstructed rainfall is recorded in AD 1540–1560 at which time higher pressure over the Caspian Sea region is inferred. 相似文献
50.
Timothy D. Jones Ian T. Lawson Jane M. Reed Graham P. Wilson Melanie J. Leng Merle Gierga Stefano M. Bernasconi Rienk H. Smittenberg Irka Hajdas Charlotte L. Bryant P. C. Tzedakis 《Journal of Paleolimnology》2013,49(2):185-204
The character and impact of climate change since the last glacial maximum (LGM) in the eastern Mediterranean region remain poorly understood. Here, two new diatom records from the Ioannina basin in northwest Greece are presented alongside a pre-existing record and used to infer past changes in lake level, a proxy for the balance between precipitation and evaporation. Comparison of the three records indicates that lake-level fluctuations were the dominant driver of diatom assemblage composition change, whereas productivity variations had a secondary role. The reconstruction indicates low lake levels during the LGM. Late glacial lake deepening was underway by 15.0 cal kyr BP, implying that the climate was becoming wetter. During the Younger Dryas stadial, a lake-level decline is recorded, indicating arid climatic conditions. Lake Ioannina deepened rapidly in the early Holocene, but long-term lake-level decline commenced around 7.0 cal kyr BP. The pattern of lake-level change is broadly consistent with an existing lake-level reconstruction at Lake Xinias, central Greece. The timing of the apparent change, however, is different, with delayed early Holocene deepening at Xinias. This offset is attributed to uncertainties in the age models, and the position of Xinias in the rain shadow of the Pindus Mountains. 相似文献