Proposers -
Estimated duration of the project: 5 years (1996-2000)
(a) in theoretical sciences:
This project is timely because coastal development involving expansion into
continental shelves in many parts of the world is taking place at an alarming
ly fast rate. For example, the Kansai International Airport in Osaka Bay,
Japan was built on an artificial island located on the continental shelf at
an average water depth of 18 m. Other international airports located on
continental shelves are currently being built in Hong Kong, Macau,
Seoul (Korea), Langkawi (Malaysia), etc.
The engineering site investigation
carried out for large coastal engineering projects is providing much new
information on the Quaternary sequences of continental shelves.
Another important source of information on the Quaternary is provided by
stability study of offshore oil platforms, the exploration and exploitation
of mineral resources including constructional materials in continental
shelves.
Research work on continental shelves in the Quaternary is largely restricted
to the developed countries with few exceptions. This is however rapidly
changing because of the importance of continental shelves as a source of food
and minerals. In many countries, research activities are undertaken by
national geological surveys, universities and research institutes. It is
also a growing trend that oceanographic research institutes are giving much
more attention to continental shelves than previously. In the shallower parts
of the continental shelves, most investigations are linked to site
investigation work carried out for coastal engineering projects. In the deep
er parts of the continental shelves, most investigations are carried out in
connection with fuel mineral exploration and exploitation. International
groups such as the Committee of the Co-ordination of Offshore Prospecting
(CCOP) in Thailand are actively involved in the exploration of marine mineral
resources on continental shelves.
The International Geosphere-Biosphere Programme (IGBP) Pages thematic studies
is actively engaged in obtaining long and high resolution records of
palaeoenvironmental changes. To date, the greatest attention has been given
to the study of palaeoclimatic record of coral reefs. It is therefore
desirable to carry out investigations on continental shelves to fill the void
existing between continental areas and the deep sea. One major advantage of
continental shelves is that the presence of Holocene deposits is certain
when a sufficient number of boreholes are available for study. Deep sea core
s on the other hand, may have their top part missing making it difficult to
distinquish between oxygen-isotope stages 1, 3 and 5. On land, the upper
part of the loess sequence also faces difficulties due to inadequacies in the
available dating methods.
Description of current activities in the field
The present state of activities in this field (include the names of institutions and responsible persons):
A list of institutions and responsible persons on a country basis is provided below:
Amongst countries at the forefront of research on continental shelves in the Quaternary, Australia may be mentioned as an example. The Australian Geological Survey Organization, universities and state geological surveys have all been very active. This has led to a much better understanding of Quaternary sea-level changes and the geological development of the Great Barrier Reef. The University of Sydney in co-operation with industry is building a sea-bed drill to improve the Quaternary stratigraphy of continental margins (see Appendix). This drill will have 100 m-penetration capability to a maximum water depth of 2000 m. In coastal cities with major infrastructural development like Hong Kong, a vast amount of site investigation information from coastal engineering is already available. This has resulted in the development of a promising line of research using Quaternary environmental changes to explain engineering properties of offshore soils on continental shelves.
Continental shelves are a finite non-renewable resource of great importance to humankind. It is not only a place where a major source of the world's food production is obtained but also an important source of mineral deposits including oil and natural gas, sand and gravel deposits, and placers including diamonds, tin and gold. It is therefore essential to obtain a better understanding of continental shelves during the Quaternary to assist in their utilization and management of human activities on continental shelves.
Objectives
The project is aimed at studying present day continental shelves down to a water depth of about 200 m in order to provide a better understanding of continental shelves in the Quaternary. Information will be sought based on the study of borehole sequences, remote sensing methods including seismic profiling. The topics to be studied will include:
Methods for achieving objectives
The research will be based on:
Previous work on the dating of continental shelf sequences have revealed a young age bias of pre-Holocene radiocarbon dates. Where boreholes have been drilled on the floor of the shelf and on coral reefs, a record of desiccated crust and dissolution surfaces related to low sea-level stands have been found. This is further supported by a vast largely untapped database of engineering soil testing results which has provided information on Quaternary environmental changes. Substantial evidence of Quaternary sea-level changes on continental shelves has already been recognised including karstic features, loess, floral and faunal remains, palaeosoils and archaeological remains. However, very little is known of their global correlation.
Previous work has already highlighted the importance of continental shelves as being critical to the understanding of marine and terrestrial processes. Unlike some of the previous IGCP projects and the IGBP where the greatest attention is given to the late Quaternary, the project will examine the entire Quaternary period. This is the main difference between the proposed project and other projects. The longer time scale examined and the multidisciplinary nature of the project should permit a much improved understanding of Quaternary processes and events on the continental shelves and provide high resolution records to assist the study of global change.
Face to face discussions with Dr P.P. Smolka, Co-leader of IGCP 341 has smoothed the path of co-operation in the field of southern hemisphere palaeoclimates during the Quaternary until the completion of IGCP 341 in 1997.
Discussions with Dr D.B. Scott, Project leader of IGCP 367 has revealed only minimal overlap. It is only in the investigation of boreholes near the present day shorelines where there is a possible overlap.
Date ___________________________ Signature ____________________________ Enclosures: