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A Philosophy of Cave Conservation
Kermode, Les The Speleological Society 1998 Journal of the speleological society of korea Vol.7 No.2
Conservation is the optimum sustained use of natural resources; therefore, cave conservation must provide not only for the protection of the character, decoration and biota of caves, but also for the means whereby people might enjoy and understand the caves that are their heritage. A cave is a natural subterranean cavity into which a man can enter to a point where daylight cannot be seen. Caves are not only interesting physical entities that provide distinctive sensory and perceptual experiences and invoke a variety of responses, but they also provide unique opportunities for scientific study. Speleology is the study of caves, and in New Zealand it attracts workers from many disciplines of the universities and government research establishments.(omitted)
Speleogenesis and Karst in New Zealand
Kermode, L.O. The Speleological Society 1997 Journal of the speleological society of korea Vol.5 No.2
The cavernous rocks of New Zealand can be grouped broadly into two main geologic types-the massive, metamorphosed, Ordovician, Mt. Arthour Marble of north-west South Island, and the stratified, bioclastic, Tertiary Te Kuiti limestones of western regions of both islands. Although much cave exploration has been carried out in both these regions, the principal study so far has involved caves and karst in the central western portion of North Island near the well-known Waitomo Caves, where some 85km of caves have been surveyed during the past 12 years by members of New Zealand Speleolgical Society.
Emberson, R.,Cody, A.,Kermode, L. The Speleological Society 1998 Journal of the speleological society of korea Vol.8 No.2
The Bullock Creek Caves are located adjacent to the usually dry river bed of Bullock Creek, which reaches the sea about a kilometer north of Punakaiki. The caves have been comprehensively written up by Rodgers(972). Under conditions of normal water flow Bullock Creek submerges where the stream meets limestone on the west side of their Punakaiki syncline. In flood conditions it overflows the first submergence and progressively floods a series of smaller submergences down valley until it comes to the caves shown on the map. All these with the exception of Wazpretti Cave and Dry Valley Cave are probably more or less flooded during and after heavy rain.(omitted)
Carroll, WM,Saida, T,Kim, HJ,Kira, J,Kermode, AG,Tsai, CP,Fujihara, K,Kusunoki, S,Tanaka, M,Kim, KK,Bates, D SAGE Publications 2013 Multiple sclerosis journal: clinical and laborator Vol.19 No.10
<P>Definite diagnosis of inflammatory demyelinating disease (multiple sclerosis (MS) and neuromyelitis optica (NMO)) may require time, but early treatment offers the opportunity to maximize patient outcomes. The purpose of this report is to provide guidance to facilitate early treatment decisions for patients with inflammatory demyelinating disease, before definitive diagnosis. Neurology experts reviewed the existing literature and clinical evidence. A treatment decision pathway was developed, defining patients for whom first-line MS disease-modifying therapies (a) are unlikely to be effective, (b) may be effective but require careful monitoring and (c) are likely to provide benefit. This algorithm seeks to ensure that patients, particularly those in Asia, receive appropriate treatment early in inflammatory demyelinating disease.</P>