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New Caledonia by Eroarome Martin Aregheore |
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INTRODUCTION
New Caledonia, a French overseas territory in the Southwest Pacific, about 1,500 km east of Australia, is an archipelago of 18,575 sq km (World Factbook), and consists of one large and one small island, and the Loyalty and Huon groups. The Main Island, New Caledonia is known as La Grande Terre. New Caledonia belongs mainly to the category of the "Mainlands" which are situated in the Southwest Pacific pre-continental zone and present an ancient volcanic sedimentary substratum with heavy relief and large areas suitable for agricultural development (Doumenge, et al. 1988). The territory also includes a number of uninhabited islets such as Huon and Surprise Islands in the D Entrecasteaux reefs, the atolls of the Chesterfield islands and Bellona reefs, Walpole Islands, Beautemps-Beaupre atolls and Astrolable reefs (Doumenge, et al. 1988) see Figure 1. The islands of New Caledonia lie between 18° and 23° S 163-169° E. The capital Noumea on Grande Terre is about 1,850 km north-east of Sydney. About 68.4 percent of the population lives in Southern Province and over half of New Caledonia's population lives in metro and greater Noumea. Since 1969, when the economic boom started, the territorys population has grown considerably. Three large ethnic groups (Melanesians, Europeans and Polynesians) are represented throughout New Caledonia. The Main Island contains about 90 percent of the population of 212,000 (Crocombe, 2001); 212,700 in mid-2000 according to SPC and 219,246 according to the World Factbook (July 2006 est.) with a 1.24% growth rate. Agriculture contributes about 2 percent of the gross domestic product (GDP), although only 1 percent of the land is arable. More than one seventh of the labour force is employed in agriculture. Cash crops include coffee, copra, and coconut palm oil. Potatoes, vegetables and maize are grown commercially while yams, taro and sweet potatoes are grown for subsistence. Yam and taro are the Melanesians staple foodstuffs. The small islands rely heavily on coconuts, copra, subsistence crops and fishing. About three-quarters of the vegetation is unique to the Main islands and is largely drought resistant. The Main Islands have rich mineral deposits of nickel, iron ore, manganese, silver, chromite and cobalt. The reserves of nickel are among the largest in the world. Phosphate deposits occur on some of the atolls and raised coral islands.
Figure 1. Map of New Caledonia Compared to other Pacific Island countries, ruminant livestock production in New Caledonia is high, although local production does not meet domestic demand, so the country still relies on the importation of meat and milk products (Table 1). Table 1. New Caledonia statistics for livestock numbers,
mutton, milk and beef production,
Pastures occupy about 15 percent of the land, and cattle, pigs and goats are raised for domestic needs. Commercial fishing includes aquaculture - shrimps, oyster and trochus -besides sea fishing. Livestock production is both subsistence and commercial. According to the 1991 Agricultural Census there were 125,461 head of cattle in New Caledonia bullocks, cows, calves and steers. Also there were 16,498 goats, 3,651 sheep, 11,425 horses and 12,523 deer. Among the cattle population few are dairy animals, however, to achieve some level of self-sufficiency in dairy products, three local companies make yoghurt, butter and cheese, from the liquid milk produced by these animals, but their output is insufficient to meet local demand (Marchal et al, 1993). Latest livestock numbers, production and import figures are shown in Table 1. |
| 2. CLIMATE AND AGRO-ECOLOGICAL
ZONES
New Caledonia is subject to the southeast trade winds which moderate the climate; it can be described as oceanic tropical: that is hot and humid without excesses. Average temperature at sea level ranges between 22 ° C and 24° C. Climate Information Like most South Pacific islands, five main categories of climate are found: (1) The tropical climate of the low lying islands, with relatively low and irregular rainfall (1200-1800 mm). (2) The tropical climate experienced on the windward slopes of the higher islands. It is always very humid with rainfall above 2000 mm at sea level, more than 5000 mm at altitude, with a short dry season during the austral winter. (3) The tropical climate found on the leeward slopes of the higher islands, where rainfall is concentrated during the hotter periods of the year and is more occasional during the cooler season (1500 2500 mm annually) with two short dry seasons (April June; September November). (4) The sub-Mediterranean climate found mostly in the southerly areas (south of Grande Terre) whose minimal temperatures are very marked frequently below 10° C, and (5) The mountain climate found in the inland valleys of Grande Terre where rainfall often reaches 6000 mm and where mists frequently occur and temperatures could fall below 10° C. There is considerable geographic and year to year variation in rainfall patterns in New Caledonia. The Central Range, the axis of which is parallel to the axis of the island, isolates a narrow strip on the East Coast, with abundant rainfall, from the western plains with semi-arid climates. An example of such differences can be seen through the comparison of the mean annual rainfall in Galarino (North-east): 4000 mm, and 45 kilometres away, in Ouaco (North-west): 800 mm. Moreover, on the West Coast, the plains are prone to droughts: evapotranspiration can be over 100 mm/month. In addition, there are considerable variations in annual rainfall, due to the random passage of depressions and cyclones; thus, in Kaala Gomen (North-west) rainfall could vary from 730 mm during a dry year up to 1650 mm in a wet year (Marchal et al, 1993). Parts of New Caledonia (e.g. the Loyalty Islands) could also be classified as "low-lying islands made up of coral masses that have emerged several dozen metres above sea level. New Caledonia Grande Terre is mountainous; the entire upland area is bordered by plains and hills that are narrow on the eastern coast and relatively wide on the western coast. It is on these coastal plains, especially the low-lying alluvial valleys that Melanesians have established their main food producing areas. |
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SOILS AND TOPOGRAPHY There is a wide range of soils, parent rocks and run off features. Drainage conditions are very different on steep slopes (East Coast and Central Range) than on gentle slopes (West Coast and Loyalty Islands). The soils have low fertility, are prone to erosion and are characteristic of mountainous islands influenced by the trade winds. Climatic differences between east and west are the cause of different soil evolution (Marchal et al, 1993). However, soils on alluvial terraces not contaminated by deposits from mine massifs (a group of mountains with a limited area) are the best in the archipelago. Soils on the basaltic or limestone plains located in the Grande Terre or in the other islands range from average to good and in some places are even excellent due to the presence of pumice stone that floats over from Vanuatus volcanoes. For details of the main physical units in New Caledonia see Doumenge, et al. (1988). Also see map. Figure 2 Map of main physical units in New Caledonia Ferralitic or ferritic soils found on ultrabasic rock are of very poor chemical composition and are physically unstable. They are deep, dark red and have a distinct tendency to harden into gravel or ferralitic crust. In spite of this, it is on this type of soil that most Melanesians, originally from Grand Terre, engage in horticulture, grow coffee trees and to lesser extent rear cattle. Another type of soil quite unsuitable for agriculture (but an important resource nonetheless) is the mangrove soil found at the mouth of the following rivers, Diahot, Koumac, Voh, Kone, Pouembout, Poya and Foa. Good quality agricultural land, and the most fertile in Grande Terre, can be identified by its largely unaltered soil formed on recent non-magnesium alluvial deposits from rivers. It is found near the coast, mainly low lying valleys both on the eastern and western sides of Grande Terre. It is here that pure deep soils ideal for open field crops or for growing shrubs are found. In general, soils in Grande Terre are not very fertile; and often very susceptible to erosion. Regular humidity on the windward coast and high up on the leeward coast causes systematic desaturation of soils. Soil differences due to climate can be observed. Magnesium is a predominant element, often associated with high concentrations of iron, nickel, chrome and cobalt. The soils are often deficient in phosphorus and sometimes also in potash. On the West Coast, chloride in the soil water relates to salted areas close to mangroves. Soils are typically shallow but with a crumbly alteration horizon. Clay valleys on the East Coast have 10-30 cm of hydromorphic horizon and often of poor drainage. The majority of soils have a gravel and hyper magnesium pattern, and thus low fertility. Alluvial soils are present too, but they are scattered and prone to flood (Marchal et al, 1993). On the leeward coast, soil acidity is marked in the dry season. On Grande Terre, a contrast exists between the windward slope (eastern coast) whose soils are deep and often very acid and the leeward slope, whose soils are fine and have quite a good chemical balance. The most obvious disadvantage of most New Caledonia soil types is that they lack chemical balance due to their ultrabasic origin. Generally, the climatic differences between east and west are the causes of different soil evolution. An agro-pedological inventory drawn up for the Grande Terre indicated that 30,000 ha were regarded as suitable for open field crops or plantation crops; 180,000 ha for pasture land; 960,000 ha for afforestation; and that 505,000 ha should be left in natural vegetation in view of their extremely poor quality and very steep slopes. |
| 4. RUMINANT LIVESTOCK PRODUCTION SYSTEMS
Beef cattle production is the main industry and features very well in New Caledonia history. However, there are other livestock such as horses, goats, sheep and deer (whose meat is exported to Japan). Two livestock production systems (smallholder and commercial) are practiced in New Caledonia. Cattle rearing occurs in all the western coastal plains and in some valleys of the eastern coast and this has often taken the place of pre-European horticulture. Most of the cattle are on European ranches while others are in Melanesian reserves. According to the 1991 livestock census there were 2,125 (cattle) stations, with 125,461 head of cattle. Since then there has been only a marginal increase in the number of cattle, 126,000 head of cattle (125,000 beef and 1,000 dairy) according to Macfarlane (1998) and a decline according to the FAOSTAT data in Table 1. Seventy percent of the farmers have less that 50 head (smallholder) and only one percent have 500 or more (commercial). Meat is the dominant output and fewer that 5 percent of the cattle are dairy cows (only 1,000 head according to Macfarlane, 1998). The predominant breeds of cattle are the Limousin, Charolais and Santa Gertrudis. Local production of beef as at 1992 was estimated at 3,220 tons and a kilogram was sold for 340 FCFP. Sale prices have increased since then but production levels have not risen as much as would have been expected. Of the total beef consumption of 4,021 tons recorded in that year, import of beef accounted for 19 percent (801 tons). Of these imports, 85 percent are frozen or refrigerated carcass and 15 percent are processed food. The cattle industry is controlled by OCEF (Office de Commercialisation et dEntreposage Frigorifique: office for marketing and frozen storage) that was created in 1963. The OCEF has a slaughtering capacity of 5000 t/year and the abattoir can process up to 1,000 t/year. The frozen storage capacity is only 75 tons. CIRAD (Centre de cooperation internationale en recherché agronomique pour le developpment) is carrying out research and development amongst others in the following areas in New Caledonia.
See CIRAD CIRAD has set up a network of 29 sample farms in the northern province, as part of a project to improve dairy cattle production in New Caledonia, and this has helped to improve the situation since 1993. For example, mean calving rates which were lower than 50 percent in 1993, rose to about 65 percent in 1995 on farms with more than 200 heads of livestock. Also on the east coast of New Caledonia, the awareness of improved livestock management techniques has increased from 5-15 percent of livestock farmers in 1992 to 25-35 percent in 1995 (CIRAD, 1995). (4) To increase feed availability to achieve all year round feeding, new hardy, drought-tolerant fodder grasses and legumes have been introduced to the ruminant producing areas covered by the CIRAD network of test farms in New Caledonia. Studies on the evaluation of rangelands for grazing ruminant livestock in New Caledonia are also being carried out by CIRAD. Also, CIRAD-EMVT has accepted to test in New Caledonia, fodder plant varieties that were bred in Australia. All these are aimed at improving the nutritional level of grazing livestock in New Caledonia. Bregeat, (1985) reported that steers offered green grass (Panicum, Sorghum and Brachiaria) every day and chopped fresh cassava roots with young Leucaena branches have daily liveweight gains of between 739 - 888 g/head/day. This indicates that well balanced diets for fattening steers could easily be produced with available green forages in New Caledonia. |
| 7. RESEARCH AND DEVELOPMENT ORGANIZATIONS
AND PERSONNEL
(1) Marchal, V., Desvals, L., and Mercier, P., CIRAD/E.M.V.T., Paita, New Caledonia. (2) Tuyienon, R., CIRAD/E.M.V.T., Province Nord, New Caledonia (3) Thierry Mennesson, CIRAD-EMVT, station de Port-Laguerre, New Caledonia. CIRAD in New Caledonia |
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REFERENCES Bregeat, C. (1985) Fattening young steers with cassava and Leucaena. Alafua Agricultural Bulletin, 11(1):115-117. Bouuzat, D. (1991) Animal Husbandry. CIRAD in New Caledonia. CIRAD (1995) Livestock Production and Veterinary Medicine Department, July, 1996. Pp52-63. Doumenge, J.P., Villenare, D. and Chapuis, O. (1988) Agriculture, Food and Nutrition in Four South Pacific Archipelagos, New Caledonia, Vanuatu, French Polynesia, Wallis and Futuna. CGPRT Centre, Jalan Merdeka 99, Bogor, Indonesia. IEMVT (1983) Centre de Port-Laguerre. Annual Report 1983, pp. 2-7. Macfarlane, D.C. (1998) Grazing livestock in the Southwest Pacific. The benefits from improved production. FAO, SAPA Publication 1998/1. Marchal, V. (1997) Systems d'alimentation des bovins en conditions tropicales seches sur la cote ouest de la province Nord (Nouvelle-Caledonia). Proceedings of a regional workshop on forage development and minewaste rehabilitation, New Caledonia, 7-11 April 1997. CIRAD-NAPPEC-SPC, pp.30-34. Marchal, V., Desvals, L., Tuyienon, R. and Mercier, P. (1993) Current status of pasture/animal production in New Caledonia. In: Sustainable beef production from Smallholder and plantation farming systems in the South Pacific. (Tony Evans, David Macfarlane and Brenda Mullen, Eds) Proceedings of a workshop held at the Islands of Efate, Santo and Malokula, Vanuatu. 2-12 August 1993. ABC printing, Milton, Brisbane, Australia, pp.42-44. WEBSITES CIRAD in New Caledonia |
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CONTACTS
This profile was written in 2002 and will be updated from time to time by: Eroarome Martin Aregheore The University of the South Pacific, School of Agriculture Alafua Campus, Apia, Samoa. Tel: 685 21 671; Fax: 685 22 933 E-mail: aregheore_m@samoa.usp.ac.fj [The profile was lightly edited by J.M Suttie and S.G. Reynolds in May 2002 and modified in May 2006] |