The Marine Ecology Research Group used detailed field surveys to assess the recovery of the inshore coastal ecosystem affected by the cataclysmic 2016 Kaikōura earthquake.

The earthquake caused seismic uplift from 0.5 to 6.4 m along 130 km of coastline and resulted in widespread die-offs of important flora and fauna and permanent losses to critical habitats.

There was much concern for the fate of diverse intertidal and subtidal communities, which include culturally and commercially important fisheries, such as pāua, and other habitat-forming species like bull kelp.

Shore-based and dive surveys tracked the abundance of over 120 marine species at 16 sites for more than six years. Findings depict major physical and ecological changes over time across sites.

The complex dynamics of recovery are described in detail in this report and clearly show that the effects from this disturbance to the Kaikōura coastal ecosystem are both significant and ongoing.

This long-term study is the first of its kind and provides a detailed data set and quantitative baselines that will help inform future coastal management decisions.

This report describes catch-at-age distributions for hake (Merluccius australis) and ling (Genypterus blacodes) from commercial fisheries for the 2021–22 (2022) fishing year, to update an ongoing time series.

These distributions are based on length data and otoliths (ear bones for ageing fish) collected by observers from commercial fishing and research trawl data.

Catch-at-age data are important for the assessment of fish stocks because they provide information on the year class strength of age classes caught and are used in analyses of trawl surveys and commercial fisheries.

The precision target (coefficient of variation) was met for analyses of hake commercial trawl Sub-Antarctic and west coast South Island fisheries but not for the Sub-Antarctic trawl survey. The target precision was met for the Chatham Rise and Sub-Antarctic ling commercial trawl fisheries, and the Sub-Antarctic trawl survey, but not for the west coast South Island commercial trawl fishery. The target precision was met for the west coast South Island and Sub-Antarctic ling longline fisheries analysed.

Further observer data collection in certain areas and months are recommended to improve the precision of the hake and ling time series in future analyses.

Increasingly frequent and intense extreme weather events such as Cyclone Gabrielle are likely to impact seafloor marine ecosystems by accelerating soil erosion and sediment transport to the ocean by rivers.

The objective of this project was to understand sediment impacts from the February 2023 Cyclone Gabrielle event on marine environments of the Hawke’s Bay and Gisborne regions to enable rapid fisheries management decisions.

We conducted two vessel surveys in June and October 2023 focusing on offshore seabed environments deeper than 15 metres. As part of these surveys we mapped selected areas of the seafloor, surveyed life on the seabed using a towed underwater camera, and obtained sediment core samples.

An ocean current and sediment transport model was designed and implemented to investigate the transport and deposition of sediments after Cyclone Gabrielle. Concentrations of suspended sediments and other parameters in the surface ocean along the east coast of the North Island were estimated from satellite images. This satellite information was used to inform the sediment transport model and to characterise the spatial extent and longevity of the offshore sediment plumes generated by Cyclone Gabrielle. A Seafloor model was used to explore impacts and recovery of seafloor ecosystems following the cyclone.

The analysis of satellite images suggest that the influence of Cyclone Gabrielle lasted approximately two to three months across the Hawke’s Bay and Gisborne coastal marine areas, with surface ocean parameters largely returning to normal by May. The concentrations of suspended sediment at the ocean surface in February were significantly elevated, but they did not exceed values typical of winter months.
Seabed mapping revealed areas of significant sediment erosion, and deposition up to about one metre in thickness, at Pania Reef, Tangoio Reef and Clive outfall area in Hawke Bay. Elsewhere, sediment core observations suggested the presence of fresh muddy deposits of up to about 15 centimetres. Swell waves were resuspending muddy sediments at shallow locations for several months after the cyclone, as was evident by the low underwater visibility during camera deployments.

The abundance and diversity of the sediment fauna sampled in Hawke’s Bay and Gisborne before (2010) and after Cyclone Gabrielle (June and October 2023) tended to increase away from the shore and into deeper waters. Sediment fauna were less abundant in June 2023 when compared with 2010, but appeared to be recovering by October 2023.

Seafloor animal and plant communities are highly likely to have been impacted by sediments at 11 of the 36 locations we surveyed using the towed underwater camera, as assessed by observations including (1) fresh mud layer on the seafloor, (2) animal/plant life in poor condition, and/or (3) absence of seaweed at shallow depths. However, for most of these locations a direct link to Cyclone Gabrielle cannot be demonstrated because no information on the distribution of seafloor organisms is available from before the cyclone. The likely exception is Wairoa Hard in Hawke Bay, where available information shows that kelp and sponges were present before the cyclone but were almost completely or completely absent after the cyclone. Whether this loss of habitat has led to reductions in associated fish populations is unclear.

Although limited by the availability of data, the ocean current and sediment transport model produced realistic predictions of suspended sediment concentrations and deposition at the seafloor. In the days following the cyclone, sedimentation in Hawke Bay was predicted to occur mainly close to shore in the western and central parts of the bay. In the Gisborne region, there was deposition of up to about 10 centimetres of sediments offshore of Poverty Bay and along a narrow band of the coast to the north near Tokomaru and Tolaga bays. These model predictions are broadly consistent with observations from the sediment core samples.

The Seafloor model showed small declines in structure-forming organisms such as sponges for Hawke’s Bay following Cyclone Gabrielle. These declines were not substantial, most likely because the region is already impacted by decades of fishing and increased sedimentation. The Seafloor model predicted weaker cyclone impacts for Gisborne than Hawke’s Bay and indicated that continued trawling may slow down recovery of seafloor communities following extreme weather events.

The lack of pre-cyclone information was a major obstacle in assessing the potential impacts of the cyclone on seabed ecosystems. Information collected as part of this project now form a valuable baseline that will inform future impact assessments in the region. Another limitation is the inability to use towed cameras to survey inshore habitats for extended periods because of poor underwater visibility. A precautionary approach could be warranted in the period following an extreme weather event until key habitats and ecosystems can be surveyed, and fish stocks and catch levels should be carefully monitored in the years following the event.

Sediment transport modelling is a promising tool for rapidly identifying areas most at risk from sedimentation following extreme weather events. However targeted sampling of sediment and water parameters under normal and flood conditions would help improve the accuracy and reliability of model predictions. The Seafloor model could be used to explore how spatial changes in fishing effort could enhance recovery following extreme weather events and could be improved through better information on the distribution of seafloor sediment and reefs and their associated animal and plant communities, particularly in the Gisborne region.

The impact of extreme weather events is made worse by decades of increased sedimentation in New Zealand’s marine environments. Addressing the long-term issue of sedimentation in marine ecosystems and the impacts of extreme weather events will require addressing the factors that have made New Zealand’s catchments more prone to erosion.

The red rock lobster supports the most valuable inshore commercial fishery in New Zealand. This fishery has been managed with catch quotas in nine Quota Management Areas (QMAs), which are usually treated as independent populations or stocks.

To estimate those quotas, each population is fully assessed every five years, requiring a lot of time and effort by a team of at least five researchers working on the review of the previous assessments and data inputs, the addition of new data, data processing, and development of a new assessment.

Every year, instead of a full assessment, a rapid update assessment is done for each of the stocks that were not assessed that year.

A rapid update repeats the previous full assessment model, only updating data inputs, which significantly speeds up the required process to provide advice about stock status in the interim years between full assessments.

This document describes the operation of the stock assessment rapid updates completed in 2023 for six stocks that can be used to guide management decisions of New Zealand red rock lobster QMAs.

For the beginning of the 2023–24 fishing year, all red rock lobster stocks evaluated were estimated to be above sustainable levels.

Popular summary of outcomes from SLMACC contract LCR30615 to Landcare Research, written by Fiona Carswell & Stella Belliss.

This research evaluated using the Task Force on Climate-related Financial Disclosures (TCFD) methodology to assess climate change risk in forestry businesses. The key benefit of the TCFD approach is that it exposes business strategy, governance and operations to risk analysis and management and focuses on understanding any financial risks. This research is the first step on what the TCFD suggests is a five-year process. This analysis can start to define the climate change risk analysis.

Keywords: Forestry, climate change, risk assessment, business risk,

Use of shallow samples to estimate the total carbon storage in pastoral soils.

Evaluation of the impact and direct effect of climate change on the productivity of New Zealand's planted forest systems.

The goal of this research is developing a theoretically robust but practically applicable methodology for valuing forests and forest land in New Zealand in the presence of carbon pricing.

This report summarises potential impacts of climate change on pests, weeds and
diseases of relevance to New Zealand’s biosecurity systems. It represents the best
current information from experts in the Crown Research Institutes and Lincoln University.

This report provides new data on soil CH4 oxidation in reverting shrubland. It describes new research, using recently acquired knowledge of the mechanisms regulating soil CH4 oxidation, to develop a practical technology for capturing emissions from housed animals, effluent ponds, and landfills.

This report, commissioned by MAF, assesses a selected range of policy instruments for mitigation of greenhouse gases in agriculture. The report assesses these options against evaluation criteria and looks at short-term options and longer term strategy.

The purpose of this report is to draw out key lessons on how science and environmental knowledge have been used in the past to achieve desired environmental outcomes. Phase Three covers the final stage and is an account of observations made during the process of discussing the research findings with the key stakeholders. three topic areas of soil erosion, pest control and nitrogen management.

Traditionally, New Zealand pastoral farmers have adapted their farming systems in response to extreme climatic events. This project will research these responses to provide information on how farmers could (and should) adapt to the extreme climatic events that may result from climate change.

Traditionally, New Zealand pastoral farmers have adapted their farming systems in response to extreme climatic events. This project will research these responses to provide information on how farmers could (and should) adapt to the extreme climatic events that may result from climate change.