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Site Factors Affecting Pinyon-juniper Occurrencein The Capulin Volcano Field Ofrnnortheastern New Mexico

机译:在新墨西哥州北部的卡普林火山场中影响松树杜松发生的场所因素

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摘要

The Capulin Volcano Field covers approximately 207,192 km2 in Union and Colfax counties in northeastern New Mexico and southernmost Las Animas county in Colorado. The geology of the area is characterized by Pleistocene and Holocene extrusive volcanic activity through sandstone, shale and limestone of the Late Cretaceous Period (Trauger & Kelly 1987). Average annual precipitation and temperature for the area is 45.2 cm. and 9.6℃ respectively (McCurdy 1994). Although, much work has been published on pinyon (Pinus spp.) - juniper (Juniperus spp.), little data have been reported on pinyon-juniper stands from the Capulin Volcano Field. Species studied in this investigation include pinyon (Pinus edulis Voss.), one-seed juniper (Juniperus monosperma Sarg.) and Rocky Mountain juniper (J. scopulorum Lemmon.) [SAF Cover Type 239 (Larson 1980)]. Although not timber producing, these stands supply posts, fuelwood, and pinyon nuts. They provide nesting platforms for birds and edge and cover for wildlife and livestock.
机译:卡普林火山场在新墨西哥州东北部和科罗拉多州最南端的拉斯阿尼玛斯县的联合县和科尔法克斯县占地约207,192平方公里。该地区的地质特征是白垩纪晚期通过砂岩,页岩和石灰岩的更新世和全新世挤压火山活动(Trauger&Kelly 1987)。该地区的年平均降水量和温度为45.2厘米。和9.6℃(McCurdy 1994)。尽管在Pinyon(Pinus spp。)-杜松(Juniper spp。)上已经发表了许多工作,但是关于Capulin火山场的Pinyon-Juniper林分的报道很少。在这项调查中研究的物种包括松子(Pinus edulis Voss。),单子杜松(Juniperus monosperma Sarg。)和落基山杜松(J. scopulorum Lemmon。)[SAF Cover Type 239(Larson 1980)]。尽管不生产木材,但这些展台供应桩,薪材和松子。它们为鸟类和边缘提供了筑巢平台,并为野生动植物和牲畜提供了掩盖。

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