2017
DOI: 10.1071/mf16219
|View full text |Cite
|
Sign up to set email alerts
|

Baseline biogeochemical data from Australia's continental margin links seabed sediments to water column characteristics

Abstract: Abstract. Surficial marine sediments are an important source of nutrients for productivity and biodiversity, yet the biogeochemistry of these sediments is poorly known in Australia. Seabed samples were collected at .350 locations in Australia's western, northern and eastern continental margins during Federal Government surveys . Parameters analysed included measures of organic matter (OM) source (d 13 C, d 15 N and C : N ratios), concentration (percentage total organic carbon, %TOC, and surface area-normalised… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
13
0

Year Published

2018
2018
2024
2024

Publication Types

Select...
9

Relationship

2
7

Authors

Journals

citations
Cited by 14 publications
(13 citation statements)
references
References 113 publications
0
13
0
Order By: Relevance
“…Many of our samples off SE Australia were collected from directly under this phytoplankton bloom (Figure 1). Conversely, the GAB samples were located to the north of this band and our samples from the NE were from relatively oligotrophic subtropical waters (Radke et al, 2017). It must be emphasized that our carbon flux data are modelled from surface chlorophyll data and depth Previous studies have shown that the bathymetric diversity gradient (BDG) for seafloor fauna is generally unimodal, with a diversity peak in the mid-bathyal (~2,000 m) in the North Atlantic…”
Section: F I G U R E 3 Key Variable Responses Using Final Rad Modelsmentioning
confidence: 95%
“…Many of our samples off SE Australia were collected from directly under this phytoplankton bloom (Figure 1). Conversely, the GAB samples were located to the north of this band and our samples from the NE were from relatively oligotrophic subtropical waters (Radke et al, 2017). It must be emphasized that our carbon flux data are modelled from surface chlorophyll data and depth Previous studies have shown that the bathymetric diversity gradient (BDG) for seafloor fauna is generally unimodal, with a diversity peak in the mid-bathyal (~2,000 m) in the North Atlantic…”
Section: F I G U R E 3 Key Variable Responses Using Final Rad Modelsmentioning
confidence: 95%
“…The non-random sampling design can be ad hoc sampling based on expert knowledge, purely opportunistic when a certain type of environmental condition becomes available, or systematic sampling. This type of sampling design was applied to many surveys [27][28][29]. For spatial predictive modeling, this method is not recommended for future studies.…”
Section: Sampling Designmentioning
confidence: 99%
“…In survey areas A-D, sediment sampling sites were selected to represent all geomorphic seabed features across the range of mapped water depths. In the survey areas E-H, sampling sites were selected using a spatially-balanced random stratified method [15][16][17] and further detailed in subsequent studies [6,29,43,44]. In total, 195 seabed sediment samples were collected and processed in the laboratory using wet sieve separation to determine percentage gravel, sand, and mud content.…”
Section: Study Region and Sediment Samplesmentioning
confidence: 99%