TEMPERATURE CONTROLS ON CORALLINE ALGAL SKELETAL GROWTH
TEMPERATURE CONTROLS ON CORALLINE ALGAL SKELETAL GROWTH
复制标题
DOI：
10.1111/j.1529-8817.2009.00780.x
复制
发表时间：
2010-04-01
影响因子：
2.9
通讯作者：
Law, Alan
中科院分区：
文献类型：
--
作者：
Kamenos, Nicholas A.;Law, Alan
许多海洋和陆地生物都有规则的生长带。在某些物种中（例如，树木），生长带几何形状的控制与环境条件有关。珊瑚藻是长寿的海洋植物，具有全球性分布，它们具有由或多或少广泛钙化的细胞组成的规则的钙化生长带。关于环境和生物对它们生长的控制知之甚少。本研究以珊瑚藻（Lithothamnium glaciale Kampum.）在8、11和15摄氏度下生长，并考虑了对藻类生长的温度控制。L.不太广泛钙化细胞内的方解石密度。冰川与夏季气温呈负相关。没有观察到温度和方解石密度之间的关系，在更广泛的钙化细胞或生长带宽本身。此外，温度控制生长在三个L。冰川菌体在过去的50年里被认为是。温度呈负相关的方解石密度在更多和更少的广泛钙化的细胞，但没有表现出一致的关系与带宽。
Many marine and terrestrial organisms lay down regular growth bands. In some species (e.g., trees), control of growth band geometry is related to environmental conditions. Coralline algae are long-lived marine plants with a global distribution that lay down regular calcitic growth bands composed of more- and less-extensively calcified cells. Little is known about environmental and organism controls on their growth. In this investigation, coralline algae (Lithothamnion glaciale Kjellm.) were grown at 8, 11, and 15 degrees C, and temperature controls on algal growth were considered. Calcite density within less-extensively calcified cells in L. glaciale was negatively correlated to summer temperature. No relationships were observed between temperature and calcite density in more-extensively calcified cells or growth-band width itself. Additionally, temperature controls on growth in three L. glaciale thalli over the last 50 years were considered. Temperature was negatively related to calcite density in more- and less-extensively calcified cells but showed no consistent relationship with band width.