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通过对单个下沉颗粒的 DNA 测序来追踪海洋中碳的输出路径。

Tracing the path of carbon export in the ocean though DNA sequencing of individual sinking particles.

机构信息

Monterey Bay Aquarium Research Institute, Moss Landing, CA, USA.

Universities Space Research Association, Columbia, MD, USA.

出版信息

ISME J. 2022 Aug;16(8):1896-1906. doi: 10.1038/s41396-022-01239-2. Epub 2022 Apr 20.

DOI:10.1038/s41396-022-01239-2
PMID:35444263
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9296562/
Abstract

Surface phytoplankton communities were linked with the carbon they export into the deep ocean by comparing 18 S rRNA gene sequence communities from surface seawater and individually isolated sinking particles. Particles were collected in sediment traps deployed at locations in the North Pacific subtropical gyre and the California Current. DNA was isolated from individual particles, bulk-collected trap particles, and the surface seawater. The relative sequence abundance of exported phytoplankton taxa in the surface water varied across functional groups and ecosystems. Of the sequences detected in sinking particles, about half were present in large (>300 μm), individually isolated particles and primarily belonged to taxa with small cell sizes (<50 µm). Exported phytoplankton taxa detected only in bulk trap samples, and thus presumably packaged in the smaller sinking size fraction, contained taxa that typically have large cell sizes (>500 μm). The effect of particle degradation on the detectable 18 S rRNA gene community differed across taxa, and differences in community composition among individual particles from the same location largely reflected differences in relative degradation state. Using these data and particle imaging, we present an approach that incorporates genetic diversity into mechanistic models of the ocean's biological carbon pump, which will lead to better quantification of the ocean's carbon cycle.

摘要

通过比较北太平洋亚热带涡旋和加利福尼亚海流中不同地点采集的表层海水和单个下沉颗粒中的 18S rRNA 基因序列群落,将表层浮游植物群落与其向深海输出的碳联系起来。在沉积物捕集器中收集颗粒,该捕集器部署在这些地点。从个体颗粒、大量收集的陷阱颗粒和表层海水中分离出 DNA。在表层水中,输出浮游植物类群的相对序列丰度因功能群和生态系统而异。在下沉颗粒中检测到的序列中,约有一半存在于大(>300μm)、单个分离的颗粒中,主要属于细胞尺寸较小(<50μm)的类群。仅在大量陷阱样本中检测到的输出浮游植物类群,因此推测在较小的下沉部分中被包裹,包含通常具有大细胞尺寸(>500μm)的类群。颗粒降解对可检测 18S rRNA 基因群落的影响因类群而异,同一地点的个体颗粒之间的群落组成差异主要反映了相对降解状态的差异。利用这些数据和颗粒成像,我们提出了一种将遗传多样性纳入海洋生物碳泵的机制模型的方法,这将有助于更好地量化海洋碳循环。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/6a795a2cfa73/41396_2022_1239_Fig7_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/5dee690ecbdb/41396_2022_1239_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/7570d9926f75/41396_2022_1239_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/0f80bd5230d7/41396_2022_1239_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/6a795a2cfa73/41396_2022_1239_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/eb13dc42c3a8/41396_2022_1239_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/2e232e3cd9bd/41396_2022_1239_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/b1c1e9df6744/41396_2022_1239_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/5dee690ecbdb/41396_2022_1239_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/7570d9926f75/41396_2022_1239_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/0f80bd5230d7/41396_2022_1239_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99cc/9296562/6a795a2cfa73/41396_2022_1239_Fig7_HTML.jpg

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