Interannual shifts in sea surface temperature and chlorophyl drive the relative abundance and group size of common bottlenose dolphins Tursiops truncatus on the Southeast Gulf of California

Karen M Zepeda-Borja, E. Morteo, Oscar R. Guzón‐Zatarain, H. Pérez-España, C. A. Delfín-Alfonso, J. Bello-Pineda
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Abstract

Despite being one of the most common odontocetes off Sinaloa (Mexican Pacific coast), basic studies on the ecology of common bottlenose dolphins (Tursiops truncatus) are scarce in the region. This study aimed to describe changes in the relative abundance, group size, and behavior of this species during 2007 – 2012. We used boat-based surveys and satellite images of sea surface temperature (SST) and chlorophyll-a (Chl-a) to model changes in dolphin relative abundance (RA) over time, using correlations in time series analyses. Overall, mean RA was 3.6 dolphins h-1 (SD = 8.0), and significantly higher RA (6.4 –16.7 dolphins h-1) occurred in 2008, 2011, 2012, which was concurrent with hydrographic effects of La Niña oceanographic conditions, as well as during the upwelling season (February – April) (SST: 17.3 – 25.0 °C; Chl-a: 3.7 – 21.4 mg m-3). Conversely, significantly lower RA values (0.5 – 3.8 dolphins h-1) occurred in 2007 and 2010 that were likely associated with El Niño effects on the biological productivity of the area (Chl-a: 0.3 – 7.6 mg m-3). We found significant correlations between monthly Chl-a and SST average values with mean bottlenose dolphins RA, and lags (22 – 29 days) in the trophic response to variations of the hydrographic parameters. Significantly larger dolphin groups were recorded during La Niña years possibly because of the higher availability of their prey. This hypothesis is supported by higher feeding frequencies (35 – 73%) observed during the upwelling seasons, especially during La Niña conditions, whereas the most frequent behavior throughout all other years was traveling (28 – 69%). Our results show that RA and group size of bottlenose dolphins inhabiting the waters off Sinaloa, Mexico, are likely influenced by the changes in hydrographic parameters, especially during extreme climatic events.
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海洋表面温度和叶绿素的年际变化决定了加利福尼亚东南湾常见宽吻海豚的相对丰度和群体规模
尽管宽吻海豚是锡那罗亚(墨西哥太平洋海岸)最常见的齿形动物之一,但该地区对普通宽吻海豚(Tursiops truncatus)生态学的基础研究很少。本研究旨在描述2007 - 2012年间该物种的相对丰度、群体大小和行为的变化。我们利用船只调查和海表温度(SST)和叶绿素a (Chl-a)的卫星图像,利用时间序列分析中的相关性来模拟海豚相对丰度(RA)随时间的变化。总体而言,平均RA为3.6海豚h-1 (SD = 8.0), 2008年、2011年和2012年的RA显著升高(6.4 ~ 16.7海豚h-1),这与La Niña海洋条件的水文效应同时发生,并且在上升流季节(2 ~ 4月)(海温:17.3 ~ 25.0°C;Chl-a: 3.7 - 21.4 mg m-3)。相反,2007年和2010年的RA值显著降低(0.5 - 3.8海豚h-1),这可能与El Niño对该地区生物生产力的影响有关(Chl-a: 0.3 - 7.6 mg m-3)。我们发现,月Chl-a和海温平均值与平均宽吻海豚RA呈显著相关,并且对水文参数变化的营养响应滞后(22 - 29天)。在La Niña年记录到的海豚群明显更大,可能是因为它们的猎物更容易获得。在上升流季节,特别是在La Niña条件下,观察到较高的摄食频率(35 - 73%)支持了这一假设,而在所有其他年份中,最常见的行为是旅行(28 - 69%)。研究结果表明,生活在墨西哥锡那罗亚海域的宽吻海豚的RA和种群规模可能受到水文参数变化的影响,特别是在极端气候事件期间。
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