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131.
132.
R. J. Stevenson 《Earth, Moon, and Planets》1987,39(3):225-236
The position of the satellite within the protonebula, the influence of the parent planet, particularly the relative effects of tidal (gravitational) as opposed to radiogenic (internal) heat generating processes, as well as the type of ice, exert a control on the evolutionary histories of the Jovian and Saturnian satellites. The landscapes of the moons are modified by surface deformational processes (tectonic activity derived from within the body) and externally derived cratering. The geological history of the Galilean satellites is deduced from surface stratigraphic successions of geological units. Io and Europa, with crater-free surfaces, are tectonically more advanced than crater-saturated Callisto.Two thermal-drive models are proposed based on: an expression for externally derived gravitational influences between two bodies; and internal heat generation via radiogenic decay (expressed by surface area/volume ratio). Both parameters, for the Galilean satellites, are plotted against an inferred product of tectonic processes — the age of the surface terrain. From these diagrams, the tectonic evolutionary state of the more distant Saturnian system are predicted. These moons are fitted into an evolutionary framework for the Solar System.Based on a paper presented at the 1985 Royal Astronomical Society of New Zealand Conference, Hamilton, New Zealand. 相似文献
133.
John W. Day Robert R. Christian Donald M. Boesch Alejandro Yáñez-Arancibia James Morris Robert R. Twilley Larissa Naylor Linda Schaffner Court Stevenson 《Estuaries and Coasts》2008,31(3):477-491
Climate impacts on coastal and estuarine systems take many forms and are dependent on the local conditions, including those
set by humans. We use a biocomplexity framework to provide a perspective of the consequences of climate change for coastal
wetland ecogeomorphology. We concentrate on three dimensions of climate change affects on ecogeomorphology: sea level rise,
changes in storm frequency and intensity, and changes in freshwater, sediment, and nutrient inputs. While sea level rise,
storms, sedimentation, and changing freshwater input can directly impact coastal and estuarine wetlands, biological processes
can modify these physical impacts. Geomorphological changes to coastal and estuarine ecosystems can induce complex outcomes
for the biota that are not themselves intuitively obvious because they are mediated by networks of biological interactions.
Human impacts on wetlands occur at all scales. At the global scale, humans are altering climate at rapid rates compared to
the historical and recent geological record. Climate change can disrupt ecological systems if it occurs at characteristic
time scales shorter than ecological system response and causes alterations in ecological function that foster changes in structure
or alter functional interactions. Many coastal wetlands can adjust to predicted climate change, but human impacts, in combination
with climate change, will significantly affect coastal wetland ecosystems. Management for climate change must strike a balance
between that which allows pulsing of materials and energy to the ecosystems and promotes ecosystem goods and services, while
protecting human structures and activities. Science-based management depends on a multi-scale understanding of these biocomplex
wetland systems. Causation is often associated with multiple factors, considerable variability, feedbacks, and interferences.
The impacts of climate change can be detected through monitoring and assessment of historical or geological records. Attribution
can be inferred through these in conjunction with experimentation and modeling. A significant challenge to allow wise management
of coastal wetlands is to develop observing systems that act at appropriate scales to detect global climate change and its
effects in the context of the various local and smaller scale effects. 相似文献
134.
Capillary gas chromatography-mass spectrometry (C-GC-MS) and Iatroscan thin layer chromatography-flame ionisation detection (TLC-FID) were used to study hydrocarbon distributions in a sediment core from Ace Lake, a saline, meromictic lake in the Vestfold Hills of Antarctica. Hydrocarbons were abundant in most core sections (up to 125/μg/g dry wt), particularly in near-surface samples, and the distributions were very complex. Major constituents were identified as phytane, 2,6,10,15,19-pentamethyleicosane, tetrahydrosqualene, a mixture of phytenes, cholesta-3,5-diene and fern-7-ene. Smaller amounts of sterenes and hopenes were also present. The predominance of the first 3 acyclic isoprenoids in sediments buried less than 30 cm is consistent with high populations of methanogenic bacteria known to be present.Phytenes were abundant in all core sections, and there was no relationship between their abundance and that of phytane which suggests that they were not derived from methanogenic bacteria. Phytadienes were minor constituents at all depths studied. An unusual feature of some distributions was the high concentrations of fern-7-ene which was the major hydrocarbon in the 20–25 cm core section. This alkene was only abundant in sediments which contained high concentrations of methanogen markers suggesting that it may also be indicative of anoxic depositional environments. A possible source might be from purple non-sulphur bacteria. High concentrations of straight-chain C29 and C34 alkenes were also found in these sediments but their origin has not been determined. Major changes in the hydrocarbon distributions with depth indicate that the depositional environment in the lake has altered dramatically since the lake was formed less than 8000 years ago. The present condition of permanent anoxic bottom waters probably developed only in the last 1000 years. 相似文献
135.
Christopher J. Stevenson Peter J. Talling Esther J. Sumner Douglas G. Masson Micheal Frenz Russell B. Wynn 《Sedimentology》2014,61(7):1982-2019
Submarine gravity currents, especially long run‐out flows that reach the deep ocean, are exceptionally difficult to monitor in action, hence there is a need to reconstruct how these flows behave from their deposits. This study mapped five individual flow deposits (beds) across the Agadir Basin, offshore north‐west Africa. This is the only data set where bed shape, internal distribution of lithofacies, changes in grain size and sea floor gradient, bed volumes, flow thickness and depth of erosion into underlying hemipelagic mud are known for individual beds. Some flows were 30 to 120 m thick. However, flows with the highest fraction of sand were less than 5 to 14 m thick. Sand was most likely to be carried in the lower 5 to 7 m of these flows. Despite being relatively thin, one flow was capable of transporting very large volumes of sediment (ca 200 km3) for large distances across very flat sea floor. These observations show that these relatively thin flows could travel quickly enough on very low gradients (0·02° to 0·05°) to suspend sand several metres to tens of metres above the sea floor, and maintain those speeds for up to 250 km across the basin. Near uniform hemipelagic mud interval thickness between beds, and coccolith assemblages in the mud caps of beds, suggest that the flows did not erode significantly into the underlying sea floor mud. Simple calculations imply that some flows, especially in the proximal part of the basin, were powerful enough to have eroded hemipelagic mud if it was exposed to the flow. This suggests that the flows were depositional from the moment they arrived at a basin plain location, and that deposition shielded the underlying hemipelagic mud from erosion. Reproducing the field observations outlined in this exceptionally detailed field data set is a challenge for future experimental and numerical models. 相似文献
136.
The obsidian hydration dating of prehistoric sites requires that each type of natural glass be identified on the basis of its elemental constituents in order that the appropriate hydration rate constants may be applied. In New Mexico, obsidian occurs in the form of in situ flows and as secondarily deposited detrital material in the sediments of ancestral watercourses. the chemical analysis of 153 geological and archaeological samples from both contexts has resulted in the identification of nine major obsidian sources. the hydration rates for New Mexican obsidians developed by different researchers are compared and evaluated in light of current knowledge on glass-water interaction. It is argued that a hydration rate developed in silica saturated solution or at 100% relative humidity are the preferred conditions for laboratory hydration rate development. 相似文献