Substrates originate from many different sources. Predominantly the sea floor is composed of fragments originating from the weathering and erosion of older rocks (either volcanic, sedimentary or metamorphic) mainly composed of silica, i.e. terrigenous (part of the earth). Organisms and ecosystems are also involved in processing and incorporating elements such as nitrogen, phosphorous, carbon and calcium into their skeletons and tissues, ultimately breaking down in the substrate. Humans also make substantial changes to the composition of the substrate.
The ocean is a major sink of carbon, including anthropogenic carbonate. During the carbon cycle vegetated marine habitats including macro-algae, seagrasses, saltmarshes and mangroves incorporate and store carbon (organic carbon). Riparian vegetation also drops into streams, forming timber snags that are important shelters for fish, or washing up on the beach as wrack that provides food and shelter for beach organisms.
The ocean’s pH tends to be basic rather than acidic, containing dissolved calcium. Calcifying organisms incorporate calcium carbonate (known as biogenic carbonate) into their skeletons, bodies, shells and tests. Calcifiers include hard corals (Hexacorallia), molluscs, foraminiferans, serpulid polychaetes, bryozoans and urchins etc. Coral reef communities account for half of all carbonate in shallow water environments and more than 25% of the carbonate buried in marine sediments. Over time the skeletons of these animals are either consolidated into limestone (e.g. rock that is over 50% calcium carbonate, such as the consolidated limestone reefs known as coral platforms) or break down into fragments on the sea floor. Calcified fragments contribute to the carbonate boulders and gravel that comprise coral rubble, to carbonate gravels (e.g. shellgrit), carbonate sands etc.). On many beaches and coastlines calcium carbonate comprises a substantial proportion of the substrate.
Ocean acidification is happening due to increasing levels of CO2 in the atmosphere, leading to an increase in the partial pressure of CO2 in seawater. This has direct consequences for the pH of the ocean, calcifying organisms, and sediments of biogenic carbonate, with major implications for erosion of coastlines composed chiefly of biogenic carbonate fragments.
Anthropogenic changes to substrate composition introduce metals, concretes, timber etc. substantially affecting their chemical makeup and the biota that colonises them.
Queensland Intertidal and Subtidal Classification Scheme
Substrate composition describes the composition of both consolidated and unconsolidated substrates and also describes the biophysical and chemical processes that formed it (as outlined in the Terrain theme).
Regional level attributes are broken into carbonate, terrigenous (land origin), chemogenic (resulting from cementation), lithic (rocky outcrops); and anthropogenic. Coffee-rock and beach rock are not distinguished from bedrock in substrate composition, however they are differentiated using the substrate consolidation attribute, being categorised with ‘intermediate’ consolidation.
Anthropogenic substrates (e.g. concrete, metal, rock walls, beach nourishment, dredge spoil etc) are distinguished using a Naturalness qualifier as they have changed from the original substrate composition.
Attributes relate to the composition of the substrate include: the source type of rock; whether it is consolidated or not; grain size of unconsolidated substrates; and the non-living composition of the substrate.
Substrate composition falls under the 'Substrate' theme of attributes for the Intertidal and Subtidal Classification Scheme. It categorises the composition of unconsolidated substrates.Attribute category table - Substrate Composition
Last updated: 23 July 2019
This page should be cited as:
Substrate composition, WetlandInfo 2019, Department of Environment and Science, Queensland, viewed 6 August 2019, .