Direct detection of phycocyanin in sediments by hyperspectral imaging.

IF 1.7 3区 地球科学 Q4 ENVIRONMENTAL SCIENCES
Journal of Paleolimnology Pub Date : 2025-01-01 Epub Date: 2024-12-30 DOI:10.1007/s10933-024-00350-y
Giulia Wienhues, Petra Zahajská, Daniela Fischer, Tobias Schneider, Martin Grosjean
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引用次数: 0

Abstract

Cyanobacteria are ubiquitous aquatic organisms with a remarkable evolutionary history reaching as far as 1.9 Ga. They play a vital role in ecosystems yet also raise concerns due to their association with harmful algal blooms. Understanding the historical patterns and drivers behind these blooms is crucial for effective ecosystem management. Lake-sediment cores are valuable natural environmental archives, recording the histories of such blooms. Among others, phycocyanin, a pigment specific to cyanobacteria, emerges as a promising biomarker for reconstructing past cyanobacterial bloom events. However, due to the physicochemical properties of phycocyanin, there is no validated method available to extract and measure this pigment from complex sediment matrix. This study explores the applicability of hyperspectral imaging (HSI), a non-destructive technique, as a novel approach for high resolution in-situ detection and quantification of phycocyanin in lake sediments. Our experiments show that phycocyanin can be detected by HSI with an absorption trough at 620 nm (relative absorption band depth, RABD620). We established a semi-quantitative calibration of the spectral index RABD620 by conducting spiking experiments with phycocyanin standard (known phycocyanin mass) on organic-rich and mineral-rich sediments of varying water contents. We also assessed potential interference from chlorophyll a, another photosynthetic pigment, ensuring the reliability of hyperspectral phycocyanin measurements. Our findings demonstrate a significant correlation (R2 ranging from 0.37 to 0.997) between the RABD620 index and associated phycocyanin amounts in organic-rich and minerogenic sediments. This indicates the potential of the spectral index to directly measure in-situ biomarker concentrations on split sediment cores. Although confounding factors such as water and chlorophyll a content can influence the spectral signal, this method offers a rapid and non-destructive approach for studying historical cyanobacterial blooms in sedimentary records. This opens promising grounds for various applications, including ecosystem-health assessment and environmental change monitoring.

Supplementary information: The online version contains supplementary material available at 10.1007/s10933-024-00350-y.

高光谱成像技术直接检测沉积物中的藻蓝蛋白。
蓝藻是一种普遍存在的水生生物,具有显著的进化史,可达1.9 Ga。它们在生态系统中起着至关重要的作用,但由于与有害藻华有关,它们也引起了人们的关注。了解这些水华背后的历史模式和驱动因素对于有效的生态系统管理至关重要。湖泊沉积物岩心是宝贵的自然环境档案,记录了这种水华的历史。其中,藻蓝蛋白,一种特定于蓝藻的色素,作为重建过去蓝藻华事件的有前途的生物标志物出现。然而,由于藻蓝蛋白的理化性质,目前还没有有效的方法可以从复杂的沉积物基质中提取和测量这种色素。本研究探讨了高光谱成像(HSI)技术作为湖泊沉积物中藻蓝蛋白高分辨率原位检测和定量的新方法的适用性。实验结果表明,在相对吸收带深度RABD620 nm处,HSI可以检测到藻蓝蛋白。采用藻蓝蛋白标准(已知藻蓝蛋白质量)对不同含水量的富有机物和富矿物质沉积物进行峰化实验,建立了光谱指数RABD620的半定量校准方法。我们还评估了叶绿素a(另一种光合色素)的潜在干扰,确保了高光谱藻蓝蛋白测量的可靠性。结果表明,富有机质和成矿沉积物中RABD620指数与藻蓝蛋白含量呈显著相关(R2为0.37 ~ 0.997)。这表明了光谱指数在直接测量分裂沉积物岩心的原位生物标志物浓度方面的潜力。尽管水和叶绿素a含量等混杂因素会影响光谱信号,但该方法为研究沉积记录中的历史蓝藻华提供了一种快速且非破坏性的方法。这为各种应用开辟了广阔的前景,包括生态系统健康评估和环境变化监测。补充信息:在线版本包含补充资料,提供地址为10.1007/s10933-024-00350-y。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Paleolimnology
Journal of Paleolimnology 地学-地球科学综合
CiteScore
3.70
自引率
9.50%
发文量
44
审稿时长
3 months
期刊介绍: The realization that a historical perspective is often useful, if not essential, to the understanding of most limnological processes has resulted in the recent surge of interest in paleolimnology. The main aim of the Journal of Paleolimnology is the provision of a vehicle for the rapid dissemination of original scientific work dealing with the reconstruction of lake histories. Although the majority of papers deal with lakes, paleoenvironmental studies of river, wetland, peatland and estuary systems are also eligible for publication. The Journal of Paleolimnology, like the subject itself, is multidisciplinary in nature, and papers are published that are concerned with all aspects (e.g. biological, chemical, physical, geological, etc.) of the reconstruction and interpretation of lake histories. Both applied and more theoretical papers are equally encouraged. The Journal of Paleolimnology will continue to be a major repository for papers dealing with climatic change, as well as other pressing topics, such as global environmental change, lake acidification, eutrophication, long-term monitoring, and other aspects of lake ontogeny. Taxonomic and methodological papers are also acceptable provided they are of relatively broad interest. New equipment designs are frequently featured. In addition to original data and ideas, the Journal of Paleolimnology also publishes review articles, commentaries and program announcements. A relevant Book Review Section is also featured.
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