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Full text: Climate-biogeochemistry interactions in the tropical ocean: data collection and legacy

<rahmann et al. 
FO 
5°S 
M77/2-076- 
M77/2-075-1 
M77/2-067-4 M77/2 5 
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M135 
SFB754 Data Legacy 
M77/2-028. 
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FIGURE 8 | Map of the Eastern Tropical South Pacific showing the location of the gravity cores and piston cores taken during cruises M77/1 (black circles), M77/2 
red triangles}), M92 (blue diamonds} and M135 (green squares) 
into 15 ml combusted (450°C, 8 h) amber—glass vials and 
at —20°C. 
FDOM was determined using 3D-—Excitation-Emission- 
Matrix (EEM) fluorescence spectroscopy followed by parallel 
factor analysis (PARAFAC). EEM spectra were obtained using 
a Cary Eclipse Fluorescence Spectrophotometer (Agilent 
Technologies) within 230-455 nm excitation wavelength range 
in 5 nm intervals and within 290-700 nm emission wavelength 
range in 2 nm intervals. All FDOM samples were brought to 
room temperature before the analyses, the measurements were 
performed under temperature-controlled conditions at 19°C 
using Cary Single Cell Peltier Accessory (VARIAN). All the 
-rontiers in Marine Science | www.frontiersin.ore 
fluorescence measurements were performed at 0.2 s integration 
ümes and 5 nm slit width on both monochromators. 
The 3D fluorescence spectra were corrected and analyzed 
by PARAFAC (Stedmon and Bro, 2008), using “drEEM toolbox 
for MATLAB” after Murphy et al. (2013). The humification 
and biological indexes were calculated after (Zsolnay et al., 
1999). CDOM samples were collected into combusted (450°C, 
8 h) 40 ml amber—glass vials. All samples were passed through 
0.2 wm polyethersulfone syringe filters (CHROMAPHIL® Xtra 
PES—45/25, MACHEREY-NAGEL GmbH & Co.KG) before 
storage at 4°C. Samples were processed within 1-90 days. 
The measurements were performed at room temperature 
3eptember 2021 | Volume 8 | Article 72330«
	        
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