Fitzroy

Fitzroy

The Fitzroy region covers an area of nearly 300,000 km2. It extends from Nebo in the north to Wandoan in the south, and encompasses the major systems of the Fitzroy, Boyne, and Calliope rivers as well as the catchments of the smaller coastal streams of the Capricorn and Curtis Coasts1.

The Fitzroy River is the largest river system running to the east coast of Australia. The Boyne and Calliope Rivers drain the southern part of the region, entering the GBR lagoon at Gladstone.

Conceptual diagrams of seagrass habitat in the Fitzroy region

MMP sites within this region are located in coastal, estuarine or fringing-reef seagrass habitats. Coastal sites are monitored in Shoalwater Bay and are located on the large shallow banks of the north western shores of Shoalwater Bay. The remoteness of this area (due to its zoning as a military exclusion zone) represents a near pristine environment, removed form anthropogenic influence. In contrast, the estuarine sites are located within Gladstone Harbour: a heavily industrialized port. Offshore reef sites are located at Monkey Beach, Great Keppel Island.

in the southern Fitzroy region tend to be intertidal, on the large sand/mud banks in sheltered areas of the estuaries. Tidal amplitude is not as great as in the north and estuaries that are protected by coastal islands and headlands support meadows of seagrass. These habitats feature scouring, high turbidity and desiccation (linked to this large tide regime), and are the main drivers of distribution and composition of seagrass meadows in this area. These southern estuary seagrasses (Gladstone, Port Curtis) are highly susceptible to impacts from local industry and inputs from the Calliope River. Port Curtis is highly industrial with the world’s largest alumina refinery, Australia’s largest aluminium smelter and Queensland’s biggest power station. In addition, Port Curtis contains Queensland’s largest multi-cargo port (Port of Gladstone) with 50 million tonnes of coal passing through the port annually.

The Shoalwater Bay monitoring sites are located in a bay which is a continuation of a coastal meadow that is protected by headlands. A feature of the region is the large tidal amplitudes and consequent strong tidal currents. As part of this tidal regime, large intertidal banks are formed which are left exposed for many hours. Pooling of water in the high intertidal, results in small isolated seagrass patches 1-2m above Mean Sea Level (MSL).

are found intertidally on the top of the fringing reefs associated with the Keppel Isles and Cannibal Island groups, however many of the reefs in the north of the region have not been surveyed. The drivers of these habitats are exposure and desiccation (intertidal meadows) and light limitation associated with wind driven resuspension .

Marine Monitoring Program

2019 -2020 Summary

Overall, the Fitzroy regional seagrass condition score remained graded as POOR in 2019–20.

There were no substantial changes from the previous year in any of the indicators, where the:

  • abundance score was poor
  • reproductive effort score was very poor
  • tissue nutrient score was poor.
Report card of seagrass status indicators and index for the Burdekin NRM region (averages across habitats and sites). Values are indexed scores scaled from 0–100 (± SE) and graded: = very good (81-100), = good (61 – 80), = moderate (41 – 60), = poor (21 – 40), = very poor (0 – 20). NB: Scores are unitless.

Within seagrass canopy water temperatures

2019–20 within-canopy temperatures were similar to the previous period and the long-term average. Maximum intertidal within-canopy temperatures exceeded 35°C for a total of 63 days during 2019–20, with the highest temperature recorded in the region at 40.5°C (RC1, 3pm 06Feb20). Daily tidal exposure was above the long‐term average in 2019–20 for the second period in four years, which may have exacerbated stresses experienced at intertidal sites.

Long-term monitoring Results:

Climate and Environmental pressures 2019-2020: 20

  • Rainfall and river discharge in 2019–20 were below the long-term average for the Fitzroy region. Exposure of inshore seagrass to turbid waters during the wet season was similar, albiet slighty higher, than the long-term average, with the coastal and estuarine sites exposed to highly turbid ‘brown’ water in most weeks. By contrast, the reef sites were exposed to predominately ‘green’ water which has lower light attenuation.

  • Annual within-canopy light availability was higher in 2019–20 than both the previous period and the long-term average for the region (Figure 9, Figure 70). The most notable change in benthic light levels occurred at Shoalwater Bay, where benthic light levels (15.5 mol m-2 d-1) were below the long-term average (18.4 mol m-2 d-1). But despite this, light levels at Shoalwater Bay were the highest among all sites in the region because they are very shallow and frequently expose to full sunlight. Daytime tidal exposure was less than the previous period but remained above the long-term average for the region, which increases the risk of desiccation stress, but in the turbid shallow waters can provide windows of light for photosynthesis.

Shoalwater Bay

Shoalwater Bay is located in the southern section of the Great Barrier Reef Marine Park World Heritage Area. The Shoalwater Bay Area covers 520 000 ha, of which approximately 50 % is marine. There is relatively little human disturbance (coastal towns and development, etc.) and it is a largely intact natural system. The region includes the most important dugong site in the southern GBR (classified as a special unique site) and is a significant wetland (classified as a Ramsar site and green turtle foraging site). Shoalwater Bay is a Dugong Protected Area (DPA), declared in January 1998 to protect key dugong (Dugong dugon) populations and habitat. The Shoalwater Bay region DPA has an ‘A’ level of protection prohibits commercial net fishing to protect dugong from entanglement in some fishing nets, as they forage and move (see GBRMPA)

Location

Shoalwater

Monitoring activity: Ongoing
Principal watchers: Seagrass-Watch HQ
Location: intertidal banks approximately 500m NW of the mouth of Ross Creek.  Wheelans Hut sites are approximately 2.5km west of Sabina Point
Site codes: RC1, RC2, WH1, WH2, WH3
Issues: freshwater and sediment runoff from the land
Comments: Due to Department of Defence restrictions, access to seagrass habitats are limited. Extensive Zostera muelleri meadows on stable mud bank. Frequented by green turtles and dugong (feeding trails common).

Status
  • Between 2009 and 2014, seagrass abundance in the bay experienced a notable decline, largely attributed to multiple years of above-average rainfall and tropical storms. From 2016 to 2018, abundance recovered; however, it declined again until 2023. Since then, it has bounced back and is currently in a GOOD state.
  • Overall, there is no significant long-term trend in abundance.
  • Seagrass species composition has remained relatively constant at RC1, however, at WH1 higher amounts of Halodule uninervis occurred during periods of decreased abundance and disturbance.
  • Seagrass species composition has changed relatively little over the past couple of years, although the amount of Halophila ovalis has fluctuated, particularly at Wheelan’s Hut

Seagrass cover, species composition and canopy height

Cover

Composition

Height

Seagrass cover, species composition and canopy height

Macroalgae and Epiphyte cover

Algae

Epiphyte

Macroalgae and Epiphyte cover

Location

Great Keppel

Monitoring: ongoing
Principal watchers: Seagrass-Watch HQ
Location: sites are located in Monkey Beach, Great Keppel Island
Site code: GK1, GK2
Issues: Land runoff
Comments: The meadows are on the intertidal sand banks at the southern end of the bay.

Status
  • Seagrass abundance has fluctuated between and within years at both sites. Over the long-term, seagrass abundance has significantly decreased at GK1, although, no trend is apparent at GK2. Seagrass abundance remains in a VERY POOR state.
  • The monitoring sites primarily consisted of H. uninervis growing on sandy substrate. Zostera muelleri was recorded in GK1 from 2008 to 2015, showing a notable increase between 2012 and 2014, followed by a decline, and has been absent since 2015.
  • The variation in seagrass species composition at the sites may indicate the dynamic nature of the intertidal sand banks.

Seagrass cover, species composition and canopy height

Cover

Composition

Height

Macroalgae and Epiphyte cover

Algae

Epiphyte
Location

Konomie

Monitoring: Established June 2025
Principal watchers: Woppaburra Rangers
Location: site are located in Considine Bay, Konomie Island
Site code: KN1
Comments: Site estalished June 2025 in collaboration with Woppaburra Rangers

Seagrass cover and species composition

Seagrass cover, species composition and canopy height

Macroalgae and Epiphyte cover

Gladstone

The Gladstone region extends from the Keppel Islands in the north, to Rodds Bay in the south. The estuarine Gladstone Harbour (Port Curtis) includes the fifth largest export port in Australia, and is presently the focus for rapid industrial expansion. The largest city in the region is Gladstone, with a population of approximately 29,288 (2006 estimate).

Location

Gladstone Harbour

Monitoring: ongoing, biannual
Principal watchers: Seagrass-Watch HQ
Location: northern and southern sections of Pelican Banks, 1 km from public boat ramp at Southend (Curtis Island)
Site code: GH1, GH2
Issues: Land runoff and industrial/port development
Comments: Extensive Zostera muelleri meadows on stable sand bank. Dugong feeding trails common.

Status
  • Seagrass abundance has fluctuated between and within years at both sites, which a period of decreased abundance at GH1 from 2014 to 2022. In 2023, seagrass abundance was on an increasing trajectory and currently is in a GOOD state.
  • Inter-annual abundances suggest a seasonal pattern of higher seagrass abundance in the late dry (spring) and lower in the late Monsoon. Over the long-term, seagrass abundance has significantly decreased at GH1, although, not trend is apparent at GH2. The site GH1 is closer to the edge of the banks is experiences occasional disturbances from drainage channels and moving sand banks.
  • Sites are dominated by Zostera muelleri with increasing compositions of Halodule uninervis and/or Halophila ovalis during periods of reduced/declining abundance.

Seagrass cover, species composition and canopy height

Cover

Composition

Height

Macroalgae and Epiphyte cover

Algae

Epiphyte

Seagrass cover, species composition and canopy height

Macroalgae and Epiphyte cover