Abstract

Sediment resuspension caused by near-bed currents mediates exchange processes between the seafloor and the overlying water column, known as benthic-pelagic coupling. To investigate the effects of sediment resuspension on microbial enzyme activities in bottom waters (<500 m), we conducted onboard erosion experiments using sediment cores taken with a multi-corer from six deep-sea sites in the northern Gulf of Mexico. We then incubated the core-top water with resuspended sediments in roller tanks to simulate bottom water conditions following sediment resuspension. Bacterial cell abundance, particulate organic matter content, and potential rates of three hydrolytic enzymes (leucine aminopeptidases – PEP; ÎČ-glucosidases – GLU, lipases – LIP) were monitored during the experimentally-generated erosion events and subsequently in the roller tanks to examine whether resuspension of deep-sea sediments enhances activities of extracellular enzymes in overlying waters. Surficial sediments were resuspended at critical shear stress velocities between 1.4 and 1.7 cm s–1, which parallel bottom water currents of 28 and 34 cm s–1. Only one of our nine cores resisted experimentally generated bottom shear stresses and remained undisturbed, possibly as a result of oil residues from natural hydrocarbon seeps at the investigated site. The most notable enzymatic responses to sediment resuspension were found for LIP activities that increased in overlying waters of all eight of our resuspended cores and remained at high levels during the roller tank incubations. PEP and GLU showed orders of magnitude lower rates and more variable responses to experimentally resuspended sediments compared with LIP. We also found a disconnect between enzyme activities and bacterial cell numbers, indicating a major role of extracellular enzymes physically disconnected from microbial cells in our experiments. Our results demonstrate that sediment resuspension may promote organic matter breakdown in bottom waters by supplying extracellular enzymes without requiring a bacterial growth response. The marked increase in LIP activity suggests that resuspended enzymes may affect the degradation of petroleum hydrocarbons, including those from the natural seeps that are abundant in the investigation area.

Highlights

  • Benthic-pelagic coupling in aquatic environments involves the exchange of dissolved and particulate matter from the sediment to the overlying water and vice versa

  • This study focused on the activities of extracellular enzymes in bottom waters following sediment resuspension, which has rarely been investigated in the deep ocean

  • Particulate organic carbon (POC): total particulate matter (TPM) ratios as a measure of the organic matter content of the resuspended material varied between 0.4% (AT357_2) and 2.5% (OC26_3), and in most cores decreased with increasing shear stress reflecting the initial resuspension of lighter POC relative to mostly inorganic matter within the TPM pool at higher shear stresses

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Summary

Introduction

Benthic-pelagic coupling in aquatic environments involves the exchange of dissolved and particulate matter from the sediment to the overlying water and vice versa. Resuspension of sedimentary matter by near-bed currents plays a key role in these exchanges, affecting ecosystem functions from nutrient fluxes to energy transfer into food webs (Graf, 1992). Due to their shallow water columns, coastal and estuarine systems are prone to sediment resuspension and such transfers (Griffiths et al, 2017), fueling microbial food webs in overlying waters (Ritzrau and Graf, 1992; Ritzrau, 1996; Ritzrau et al, 1997; Boetius et al, 2000; Ziervogel and Arnosti, 2009; Ziervogel et al, 2016). Budget calculations revealed that the amount of particulate and dissolved organic matter released through resuspended sediments in the deep ocean could close budget gaps between the carbon supplied to the benthos through sinking organic matter and the prokaryotic carbon demand in the deep-sea (Pfannkuche, 1993; Boetius et al, 2000; Baltar et al, 2010)

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