2016
DOI: 10.2112/jcoastres-d-14-00223.1
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Phytoplankton Pigments in Maryland Coastal Bay Sediments as Biomarkers of Sources of Organic Matter to Benthic Community

Abstract: BioOne Complete (complete.BioOne.org) is a full-text database of 200 subscribed and open-access titles in the biological, ecological, and environmental sciences published by nonprofit societies, associations, museums, institutions, and presses.

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Cited by 7 publications
(8 citation statements)
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“…Particularly, the pigments from diatoms and dinoflagellates (Fuco and Peri) are generally more labile than those originating from cryptophytes (Allo), cyanobacteria (Zea), and green algae (Lut; Leavitt & Carpenter 1990;Leavitt 1993;Chen et al 2015). This finding suggests that the main sources of phytoplankton-derived OM are diatoms, cyanobacteria, cryptophytes, chrysophyceae, prasinophytes, and dinoflagellates.…”
Section: Source Of Phytoplankton Pigments In Surface Sedimentsmentioning
confidence: 99%
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“…Particularly, the pigments from diatoms and dinoflagellates (Fuco and Peri) are generally more labile than those originating from cryptophytes (Allo), cyanobacteria (Zea), and green algae (Lut; Leavitt & Carpenter 1990;Leavitt 1993;Chen et al 2015). This finding suggests that the main sources of phytoplankton-derived OM are diatoms, cyanobacteria, cryptophytes, chrysophyceae, prasinophytes, and dinoflagellates.…”
Section: Source Of Phytoplankton Pigments In Surface Sedimentsmentioning
confidence: 99%
“…However, the abundance of taxonomically diagnostic carotenoids in the sediments cannot be directly used to estimate the contribution of the different algal groups because stability varies substantially among the pigments. Particularly, the pigments from diatoms and dinoflagellates (Fuco and Peri) are generally more labile than those originating from cryptophytes (Allo), cyanobacteria (Zea), and green algae (Lut; Leavitt & Carpenter 1990;Leavitt 1993;Chen et al 2015). Although Fuco is a highly labile phytopigment, it remains as the most abundant accessory pigment in the surface sediments.…”
Section: Source Of Phytoplankton Pigments In Surface Sedimentsmentioning
confidence: 99%
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“…On the other hand seasonal variation in POC in sediments was found in Adventfjorden (Svalbard) station located in shallow zone (at 40 m depth) influenced by the nearby river outlet (Zajączkowski et al 2010;Pawłowska et al 2011). The higher CPE resulting from increased phaeophytin, products of Chl a degradation, may indicate that in the late summer the organic matter produced in the water column reaches the bottom after being grazed by mesozoplankton (Chen et al 2016). However, according to Krajewska et al (2017) sum of Chl a and its derivatives (CPE) is a much better indicator of pelagic primary production than only Chl a content.…”
Section: Benthic Response To Seasonal Variability In Kongsfjorden Ecomentioning
confidence: 99%