Henkel Sarah K, Nelson Walter G
Hatfield Marine Science Center, Oregon State University, Newport, OR 97365,
Western Ecology Division, National Health and Environmental Effects Research Laboratory, U.S. Environmental Protection Agency, Newport OR 97365, USA.
J Biogeogr. 2018;45(12):2701-2717. doi: 10.1111/jbi.13451.
We assessed whether currently described marine biogeographic boundaries apply to shelf macrofauna and which environmental drivers were most associated with species differences among regions.
Pacific coast of North America from the Strait of Juan de Fuca in Washington to the California-Mexico border.
Van Veen grab samples were collected from soft sediment 28-138 m deep and sieved using 1 mm mesh. Spatial patterns of species richness, diversity, and abundance were examined in relation to latitude and environmental parameters (temperature, salinity, dissolved oxygen, sediment % fines, and total organic carbon). Analyses of latitudinal distribution patterns of individual species were combined with multivariate analyses of community composition to determine biogeographic and habitat boundaries for mid-depth continental shelf macrofauna.
Species richness, diversity, and abundance significantly decreased with increasing latitude, primarily between 32 and 40° N. There were positive associations of richness, diversity (H'), and abundance with upwelling index, sediment % fines, and TOC (<2%). Temperature and DO also were significant for richness and H' but not abundance. Assessment of individual species ranges found major faunal transitions at latitudes 33-34°, 37°, 44°, and 46-47°. Major assemblage differences were found at 34.5°, and 42°. Within each latitudinal region, significantly different macrofauna communities were found in sediment with <5% fines.
The biogeographic boundaries proposed under the Marine Ecoregions of the World schema are more closely aligned with shelf fauna distributions than those developed using west coast rocky intertidal communities. However, the proposed province boundary at Cape Mendocino is not apparent in the shelf macrofauna, and a transition appears to occur closer to the Oregon-California border. Further, the shelf macrofauna indicate the Channel Islands should be a separate subregion from mainland southern California Bight. Multivariate community analyses minimizing the impact of rare species appeared more useful in determining macrofaunal community biogeographic boundaries than analysis of individual species range endpoints, which are strongly influenced by uncommon species.
我们评估了当前所描述的海洋生物地理边界是否适用于陆架大型底栖动物,以及哪些环境驱动因素与各区域间的物种差异最为相关。
从华盛顿州的胡安·德富卡海峡到加利福尼亚 - 墨西哥边境的北美太平洋海岸。
使用Van Veen抓斗从28 - 138米深的软质沉积物中采集样本,并用1毫米筛网进行筛分。研究了物种丰富度、多样性和丰度的空间格局与纬度及环境参数(温度、盐度、溶解氧、沉积物细粒百分比和总有机碳)之间的关系。将单个物种的纬度分布模式分析与群落组成的多变量分析相结合,以确定中深度大陆架大型底栖动物的生物地理和栖息地边界。
物种丰富度、多样性和丰度随纬度增加而显著降低,主要在北纬32°至40°之间。丰富度、多样性(H')和丰度与上升流指数、沉积物细粒百分比和总有机碳(<2%)呈正相关。温度和溶解氧对丰富度和H'也有显著影响,但对丰度无显著影响。对单个物种分布范围的评估发现,在纬度33 - 34°、37°、44°和46 - 47°处存在主要的动物区系转变。在34.5°和42°处发现了主要的群落差异。在每个纬度区域内,在细粒含量<5%的沉积物中发现了显著不同的大型底栖动物群落。
在“世界海洋生态区”模式下提出的生物地理边界比使用西海岸岩石潮间带群落所确定的边界更符合陆架动物的分布。然而,在门多西诺角提出的省界在陆架大型底栖动物中并不明显,转变似乎发生在更靠近俄勒冈 - 加利福尼亚边境的地方。此外,陆架大型底栖动物表明海峡群岛应是南加利福尼亚湾大陆架以外的一个单独子区域。与分析受罕见物种强烈影响的单个物种范围端点相比,将稀有物种影响降至最低的多变量群落分析在确定大型底栖动物群落生物地理边界方面似乎更有用。