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Sự Loại Bỏ Lượng Mưa Ngắn Hạn Thay Đổi Phản Ứng Của Vi Sinh Vật Đối Với Độ Ẩm Đất Ở Một Rừng Nhiệt Đới Ẩm
Tóm tắt
Nhiều rừng nhiệt đới ẩm, nơi chứa một phần tư trữ lượng carbon sinh khối trên cạn toàn cầu, sẽ trải qua những thay đổi về chế độ lượng mưa trong thế kỷ tới. Phản ứng của vi sinh vật trong đất đối với sự thay đổi lượng mưa có khả năng là một phản hồi quan trọng đối với chu trình carbon của hệ sinh thái, nhưng các cơ chế sinh thái đứng sau những phản ứng này vẫn chưa được hiểu rõ. Chúng tôi đã khảo sát ảnh hưởng của lượng mưa giảm đến số lượng, hoạt động, và thành phần cộng đồng vi sinh vật trong một thí nghiệm loại bỏ lượng mưa kéo dài 6 tháng tại Trạm Sinh học La Selva, Costa Rica. Sau đó, chúng tôi đã đánh giá những tác động kéo dài của các phương pháp điều trị độ ẩm đất trong thực địa bằng cách tiếp xúc đất với một gradient độ ẩm đất được kiểm soát trong phòng thí nghiệm trong 4 tuần. Tại hiện trường, các phản ứng về thành phần và chức năng đối với lượng mưa giảm phụ thuộc vào điều kiện ban đầu, phù hợp với mức độ biến thiên không gian lớn trong các khu rừng nhiệt đới. Tuy nhiên, việc can thiệp về lượng mưa đã thay đổi một cách đáng kể các phản ứng chức năng của vi sinh vật đối với độ ẩm đất. Các cộng đồng đã trải qua hạn hán trước đó thể hiện tỷ lệ hô hấp cao hơn trên đơn vị sinh khối vi sinh vật trong tất cả các điều kiện và thải ra CO2 nhiều hơn đáng kể so với đất đối chứng ở độ ẩm đất thấp. Những mẫu chức năng này gợi ý rằng sự thay đổi trong sinh lý của vi sinh vật có thể tạo ra phản hồi tích cực đối với nồng độ CO2 trong khí quyển đang gia tăng nếu các rừng nhiệt đới ẩm trải qua các mùa khô kéo dài hơn hoặc mạnh mẽ hơn trong tương lai.
Từ khóa
#vi sinh vật #độ ẩm đất #rừng nhiệt đới ẩm #phản ứng sinh thái #carbon khí quyểnTài liệu tham khảo
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