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Cơ chế di chuyển ngược dòng của cá vược ôn đới thanh nữ Lateolabrax japonicus tại cửa sông Yura có phân tầng
Tóm tắt
Các điều kiện thủy văn và phân bố của cá vược ôn đới thanh nữ Lateolabrax japonicus được quan sát vào đầu mùa xuân từ năm 2009 đến năm 2012 tại cửa sông Yura, nơi có sự phân tầng cao do thủy triều nhỏ và sự xâm nhập của nước biển vào lớp đáy của sông dưới dạng một mảnh muối. Trong cả bốn năm được nghiên cứu, sự mở rộng về phía thượng nguồn của sự phân bố của chúng trùng khớp với thời điểm xâm nhập của mảnh muối từ phần dưới lên phần trên của cửa sông, cho thấy rằng cá non đã sử dụng sự xâm nhập của mảnh muối để di chuyển lên thượng nguồn vào đầu mùa xuân. Tuy nhiên, cá non đôi khi vẫn ở khu vực gần bờ ngay cả khi mảnh muối đã xảy ra, cho thấy rằng các yếu tố kích thích khác cũng có thể cần thiết. Do đó, chúng tôi đã đánh giá tác động của nhiệt độ lên hành vi di cư ngược dòng. Mối quan hệ giữa nhiệt độ trung bình mà chúng trải qua từ khi nở cho đến khi bắt đầu di chuyển lên và tuổi trung bình của mỗi nhóm cá trong quá trình di cư ngược dòng phù hợp với quy luật nhiệt độ tích lũy hiệu quả. Hầu hết các nhóm cá đã di chuyển lên thượng nguồn khi đạt nhiệt độ tích lũy hiệu quả khoảng 500 °C-ngày. Điều này cho thấy rằng nhiệt độ cao hơn sẽ dẫn đến khoảng thời gian ngắn hơn trước khi di chuyển ngược dòng.
Từ khóa
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