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Particles in the ocean play an important role in marine biogeochemical cycles1. Most of the properties of particles, such as size, mineralogy, and composition, can change profoundly from one geological or hydrographical setting to another2. In addition, the distributions of elements in the ocean are also associated with the life cycle of marine phytoplankton: growth, death, sinking, and re-mineralization3,4. Marine particles span at least 4 orders of magnitude in size, ranging from submicron particles to large aggregates (>5 mm). Most particles are biologically derived, from processes such as viral lysis, exudation, secretion, fecal pellet production, etc. Other particles are formed from physical coagulation of cells, cellular debris, or lithogenic materials1. Various chemical and biological characteristics of particles control both the geochemical cycles and biological processes occurring on and within the particles4,5,6. These particles are important habitats as well as food sources for some organisms, such as zooplankton or saprotrophs. Accordingly, the fate of particles is often related to their size, which can be modified by biological processes on and around particles.
Sampling marine particles usually requires filtration, but this approach introduces a certain ambiguity in identifying the properties of particles, since marine particles are not homogenous in composition and size. Suspended particles, mainly composed of small and low density particles that are almost permanently in suspension, are mixed with varying amounts of larger and denser particles in suspension only for a short period of time, depending on hydrodynamic conditions7. The first reports of the trace metal composition of plankton samples were collected by plankton tows or suspending plankton nets on a research vessel8. The authors often found metal particles and paint chips in samples, suggesting a severe problem of contamination during marine particle sampling for chemical analysis. Other efforts include net towing by rubber rafts or using a polyvinyl chloride (PVC)-hand winch3. The difficulty of reliable sampling of particles makes progress in our understanding of the chemical composition of marine particles more difficult, especially for trace elements. As such, most crucial information on the concentration of trace elements in phytoplankton has come from culture studies9,10. This recognition has motivated marine scientists to create new methods for studying particles in the sea over the past thirty years11.
Oceanographers have used various sampling techniques, including shipboard filtration, in situ filtration, and sediment traps11. The processing of large volumes of sea-water to collect non-contaminated samples can be challenging, especially for open ocean and deep waters in which the particle concentrations are very low (0.001 - 0.1 mg/L). It is also necessary to filter large volumes of sea-water to obtain an adequate quantity of particles to measure trace metal concentrations. Some researchers have used the size-fractionation method to separate suspended particles from sinking particles. However, particle size, porosity, density, and shape can all influence particle sinking velocities. Sediment traps are not practical tools to collect suspended particles, since those are designed for sinking particles. Therefore, it is important to develop sampling and treatment methods that can collect sufficient quantities of suspended particles with minimal contamination. Hence, size-fractionation by in situ filtration is still a promising tool in the oceanographer's sampling toolbox, since it can reveal critical information on marine particle dynamics. Here, we describe a successfully tested trace-metal-clean, multi-layer gravity filtration sampling apparatus, which can treat large volumes (120 - 240 L) of seawater on board in one pass from polytetrafluoroethylene (PTFE) coated water sampling bottles in a multi-bottle sampling array. This sampling apparatus uses acid-washed synthetic nylon nets in sequence, and the nets are enclosed within a polycarbonate container to gently collect size-fractionated suspended matter and phytoplankton12,13,14,15 (Figure 1). The aim of this work is to provide a better tool for studying the metal-particle associations and their reaction dynamics in marine environments, and improve our understanding of the fate of a wide variety of planktons, particles, and trace metals in these environments.