Doctoral Thesis
Refine
Year of publication
- 2009 (2) (remove)
Document Type
- Doctoral Thesis (2) (remove)
Language
- English (2) (remove)
Has Fulltext
- yes (2)
Is part of the Bibliography
- no (2)
Keywords
- Agenda 21 (1)
- Akteurzentrierter Institutionalismus (1)
- Caribbean region (1)
- Cayman Trog (1)
- Cuba (1)
- Geodynamik (1)
- Geologie (1)
- Governance (1)
- Great Caribbean Arc (1)
- Hispaniola (1)
- Institutionalisierung (1)
- Jamaika (1)
- Karibik (1)
- Karibik <Nordwest> (1)
- Karibische Flutbasaltprovinz (1)
- Kuba (1)
- Oriente (1)
- Plattentektonik (1)
- Polen (1)
- Protokaribik (1)
- Ressourcenmanagement (1)
- Tektonik (1)
- Transformationsländer (1)
- Vietnam (1)
- geology (1)
- plate tectonics (1)
- tectonic reconstruction (1)
Institute
- Institut für Geographie und Geologie (2) (remove)
The Caribbean is a geologically complex region with several different plate boundary interactions. Geodynamic reconstructions of the northwestern Caribbean region have been particularly controversial in terms of the number of arcs, subduction polarity, and timing of collision. This thesis develops a refined tectonic reconstruction for the northwestern Caribbean based on a review of geological data of Cuba and a regional analysis within the northwestern Caribbean context. With regard to plausibility, significant emphasis was put on the degree and qualitiy of visualization. Three crustal sections across key areas in western, central, and eastern Cuba have been constructed in order to conduct an evolutionary interpretation in three dimensions. Western and central Cuba constitute an orogenic belt resulting from the collision of a mid- to Late Cretaceous volcanic arc - the "Great Caribbean Arc" - with the southern paleomargin of North America. The collision process apparently started in the Campanian, but major north- to northeast-directed thrusting processes at the southern Bahamas margin culminated during the Paleocene. A continous southwest-dipping polarity of the "Great Caribbean Arc", at least from the Aptian-Albian, can be infered from (1) its Late Cretaceous approach towards the North American margin, (2) the magnitude of top to the north directed tectonic transport in the Cuba orogenic belt, and (3) the internal structures of the metamorphic fore-arc assemblages and their evolution on the north side of the arc. An Early Cretaceous southwest-dipping origin of the "Great Caribbean Arc" along the northern fringe of the Chortís Block appears to be in all probability. This concept provides a link between (1) middle Late Cretaceous collision processes along the Matagua suture zone, (2) the Turonian termination of "Great Caribbean Arc"-activity on Jamaica, and (3) the late Campanian onset of collision in the Cuba orogenic belt. The collision of the "Great Caribbean Arc" with the Bahamas margin hampered relative northward motion of the Caribbean Plate from the late Campanian onward. Continued northward push finally resulted in the commencement of north-dipping subduction. Late Cretaceous commencement of north-dipping subduction was accompanied by superposition of oceanic crust and large-scale north-directed gravity sliding on the upper plate, as documented by ophiolitic slide-masses and Maastrichtian olistostromes in eastern Cuba (Nipe - Cristal and Moa Baracoa ophiolite massifs) as well as on Jamaica (ophiolites of the Bath-Dunrobin Complex) and the southern peninsula of Hispaniola. Progress of north-dipping subduction was responsible for the emergence of a Paleocene to Middle Eocene volcanic arc which spanned the northwestern Caribbean along the southern boundary of the Yucatán Basin while the Chortís Block and the Nicaragua Rise were still in a paleoposition to the south of the Maya Block. North-dipping subduction and the associated volcanic arc isolated the Yucatán Basin from its original affiliation to the Caribbean Plate. Relative northward motion of the Caribbean Plate and activity of the Paleogene volcanic arc stopped after the Eocene arrival of thickened oceanic crust of the Caribbean Large Igneous Province at the north-dipping subduction zone. After the late Early Eocene commencement of spreading at the Mid-Cayman Rise, North America - Caribbean relative motion was taken up along the sinistral Oriente Fault with estimated amounts of 800 to 1000 km offset since the Middle Eocene. This transform margin dissmembered the northwestern Caribbean extend of the Paleocene to Middle Eocene volcanic arc. Its eastern bend was uncoupled in the course of this process and may be represented by the Aves Ridge. South-central Hispaniola can be restored to a Middle Eocene position to the south of eastern Cuba, which accounts for an approximate Cenozoic displacement of 200 to 300 km. Therefore, most of the western prolongation of the Oriente Fault must be accommodated at the northern bounding-faults of the southern peninsula of Hispaniola. The proposed synthesis is in clear accordance with the paradigm of plate tectonics, corroborating its capability to incorporate even a complex region like the Caribbean.
In 1992, the international regime 'Agenda 21' was agreed upon. Accordingly, countries worldwide have been undergoing reforms in their water management into Integrated Water Resources Management (IWRM). The implementation is promoted by international actors. The main institutional aspects of IWRM are the river basin approach, clear property rights allocation, and application of economical instruments. In former centrally planned economies, the process of IWRM implementation has been coincided with transformation for the market economy. The implementation of institutional aspects of IWRM in countries under transition is connected with high transaction costs. Against this background, the comparative empirical study was initialised in order to analyse institutional change of water management towards IWRM in Vietnam and in Poland. Two models of river basin organisations were examined. Consequently, pros and cons of decentralised polycentric and hierarchical unicentric river basin organisations have been evaluated. Formal institutions were studied with the use of an in-depth review of legislation in Vietnam and in Poland. The EU Water Frame Directive (EU WFD) and other international policies were also examined. For the empirical study in Vietnam and in Poland, actors were interviewed as experts. The results of the study on both countries were discussed separately, and conclusions were drawn in a comparative manner. Water management reforms towards IWRM in Vietnam and in Poland have been generating multi-level governance processes including international, national and sub-national levels. The implementation of IWRM in Vietnam is supported by international donor agencies. In Poland, the implementation of the EU WFD is coordinated by the European Commission in a hierarchical manner. In comparison to international joint-development projects in Vietnam, the European Commission enforces international IWRM policy more effectively. Since the resumption of ODA in early 1990s, water resources management has been institutionalised in Vietnam by international support. In 1998, a Water Law was established in Vietnam. The intended separation of water resources management from water service provisions caused fragmentation between the Ministry of Natural Resources and Environment, and the Ministry of Agriculture and Rural Development, respectively. This ‘silo-effect’ has been intensified by the competition for international ODA. The power struggles affect even agencies within ministries. Polycentric river basin committees have been established as entities subordinated to the Ministry of Agriculture and Rural Development, as well as the Ministry of Natural Resources and Environment. However, because of weak property rights allocation and the absence of administrative powers, the river basin organisations work ineffectively. The river basin has not yet been established as a sub-national area of political action. Decisions sustained to be made at central level and are affected by the information problem due to largely centralised organisations of Vietnamese water management. The sub-national level is characterised by very low planning and management capacities. In Poland, unicentric river basin organisations were established in 1991. They are aligned with hydrological borders. Water resources planning and management are carried out according to river basins and water regions in order to implement the EU WFD. The river basin has been established as a new area of decision-making. Conflicts between local-governments have been resolved after the reforms. Nevertheless, spatial management planning, environmental protection planning, water service delivery, etc., are further carried out by local self-governments. To integrate water resources planning and management with these services, horizontal coordination is of critical importance. However, this is hampered by problems of ‘spatial fit’. Moreover, a high degree of horizontal cross-border communication increases information problems in hierarchical organisations. Thus, features of polycentric governance models become increasingly important in order to fully implement the EU WFD in Poland.