North East SMR

Location and physical characteristics

Coastline length (km) 307
Sea area (km2) 3,153
Deepest point (m) 224
Shallowest point (m) coastline
Average depth (m) 63
Tidal range (m) 2.6 – 4.0
Salinity 34.44 – 34.82
Sea surface temperature (°C):    7.1 – 14.3



The North East SMR is located in the northern North Sea and has a rather uniform coastline (Figure 1). The long-term monitoring site at Stonehaven shows annual variation and periodic large, short-term reductions in salinity at the surface. Overall the freshwater input is low in this region except for the rivers Dee, Don and North Esk. Tidal currents are mainly directed parallel to the coast and the residual flow is southward along the coast. The wave climate in this region is influenced by conditions in the North Sea, which can lead to long fetch because of the wind direction. The relatively straight coastline provides few natural places of shelter from these waves.

Sand is the main seabed sediment in the North East SMR, with gravelly-sand in the northern part. Off the Aberdeenshire coast Pleistocene deposits vary from soft red-brown, grey-brown and pink-grey muds, to compact grey clays with scattered pebbles, which probably represent glacial tills. The soft muds at the top of the sequence were deposited during the decay phase of the last ice sheet in the region.

Devonian (Old Red Sandstone) and Permo-Triassic (New Red Sandstone) rocks extend offshore along the coastal margin of the Moray Firth south, covering most of the Dalradian rocks seen onshore, except in the section between Aberdeen and Stonehaven. These strata comprise sandstones, conglomerates, mudstones and cherts deposited in continental, often fluvial environments.

Productive

The North East SMR contains the largest white fish market in Scotland at Peterhead and the main port for the North Sea oil and gas industry, Aberdeen. A total (demersal, pelagic and shellfish) of 170,227 tonnes was landed into Peterhead and other small ports covered by the Peterhead Marine Scotland Fisheries Office in 2018. These ports have provided services to both the fishing and oil and gas industries for many years, the fishing industry having a longer history than oil and gas which started to develop in the 1970s.

The Productive Assessment has been undertaken, with a focus on 2014 – 2018, on a sectoral basis. For a number of Sectors, including aquaculture, oil and gas, and aggregates, there was no activity within the North East SMR during the period 2014 – 2018.

However, for many sectors, there were changes over the period 2041 – 2018 (Figure 2).



Figure 2: Changes that have taken place in the North East SMR by Sector. Although the period 2014 – 2018 inclusive has been used where possible, there are some entries when a slightly different time period has been used.

Pressures from human activities

As part of SMA 2020, an assessment of the main pressures from human activities in each of the Scottish Marine Regions and Offshore Marine Regions was undertaken through a MASTS-led workshop. The process and outcomes are presented in detail in the Pressure from Activities section. Five main pressures identified for the North East SMR ordered as per the MASTS-led Pressure Assessment Workshop were:

Priority [1] Pressure (FeAST classification) [2] Main healthy and biologically diverse components affected [3] Main contributing FeAST activity /activities to pressure [4] Associated productive assessments [5]
1 Removal of target species (including lethal)
  • Fishing - Bottom otter trawling and pair trawls (OTB, OTT, PTB, TB, TBN)
  • Fishing - Creeling and potting (FPO)
  • Fishing - Scallop dredging (DRB)
2 Removal of non-target species (including lethal)
  • Fishing - Bottom otter trawling and pair trawls (OTB, OTT, PTB, TB, TBN)
  • Fishing - Creeling and potting (FPO)
  • Fishing - Scallop dredging (DRB)
3 Physical change (to another seabed type)
  • Extraction – Dredging (capital and maintenance)
  • Fishing - Scallop dredging (DRB)
4 Surface/Sub-surface abrasion/penetration
  • Extraction – Dredging (capital and maintenance)
  • Fishing - Bottom otter trawling and pair trawls (OTB, OTT, PTB, TB, TBN)
  • Fishing - Creeling and potting (FPO)
  • Fishing - Scallop dredging (DRB)
5 Underwater noise
  • Extraction – Dredging (capital and maintenance)
  • Fishing – any gear
  • Infrastructure - Coastal (ports, marinas, leisure facilities)
  • Military activities – Sonar use
  • Shipping
  • Tourism & recreation

Clean and safe

The assessments cover eutrophication, hazardous substances, marine litter, noise, and microbiology and algal toxins which have the potential to have an impact on habitats and species as well as being a consequence of human activity. Although sources of litter or contaminants may be local, there are cases when the source is some distance from the impacted area. The main findings for the North East SMR are:

Eutrophication

Highest nutrient inputs came from the most populated areas of Scotland including the North East, but were stable. However, chlorophyll and winter nutrient concentrations were low (below assessment thresholds) and there was no trend. There were no dissolved oxygen data for this SMR. Overall the North East SMR showed no evidence of eutrophication as a consequence of nutrient enrichment.

Hazardous substances

Hazardous substances (polycyclic aromatic hydrocarbons (PAHs), polychlorinated biphenyls (PCBs), polybrominated diphenyl ethers (PBDEs) and heavy metals (Hg, Cd and Pb)) assessments in sediment and biota (fish and shellfish) were undertaken at the scale of the five Scottish biogeographic regions: Atlantic North-West Approaches, Irish Sea (Clyde and Solway), Minches and Western Scotland, Scottish Continental Shelf and Northern North Sea. The North East SMR is in the Northern North Sea biogeographic region. Contaminant concentrations in the Northern North Sea region were generally above background but below concentrations where adverse effects could occur. In addition, concentrations in sediment and biota were stable or declining for all hazardous substances measured. There were no biota or sediment stations in the North East SMR. There was an increasing trend in mercury inputs to the North East SMR.

A number of biological effects were also measured and assessments undertaken at the scale of the five Scottish biogeographic regions. Assessment of imposex in dog whelks, an indicator of TBT contamination, included two sites in the North East SMR. Results from both sites indicated that concentrations of TBT in the marine environment are not causing significant harm (< Environmental Assessment Criteria). The remaining biological effects measurements included in the assessment are from fish and there are no fish sampling sites in the North East SMR. At the biogeographic scale, the other contaminant-specific biological effects (PAH bile metabolites and 7- ethoxyresorufin O-deethylase (EROD) activity) in the Northern North Sea were consistent with the hazardous substances and showed a limited exposure to contaminants. The Northern North Sea showed an increase in fish disease in some years but this could not be linked to exposure to contaminants.

Marine litter

Due to the lack of assessment criteria for marine litter, beach litter and microplastic, status assessments were not possible. However, litter and microplastics are present in all SMRs, including the North East SMR. The North East SMR has a relatively low concentration of microplastics in surface water (< 5,000 microplastic particles per km2 of sea surface).

Seafloor litter was assessed at the scale of the biogeographic regions; the North East SMR is included in the Northern North Sea region. The evidence indicates that there is no consistent trend in seafloor litter density between 2012 to 2018 inclusive for the Northern North Sea.

Beach litter was also assessed in the North East SMR. Apart from beach litter indicators associated with wet wipes, angling and smoking, most other categories suggest improving beach conditions.

Noise

There are limited noise data for the North East SMR. Continuous noise data were collected in 2013 and 2014 as part of the East Coast Marine Mammal Acoustic Study (ECOMMAS). Overall, the continuous noise levels at each site, including those in the North East SMR, are broadly similar. Noise levels in the 125 Hz one-third octave band are predominantly within the range 80 – 120 dB re 1 μPa rms, and the modes of these distributions lie between 84 – 95 dB re 1 μPa rms. Very few impulsive noise data were reported for the North East SMR. It is not possible to do a status assessment as there are no assessment criteria to say what levels of noise are harmful, and there are not enough years of data to carry out a trend assessment.

Microbiology

A number of bathing waters in the North East SMR are assessed according to levels of Escherichia coli and intestinal enterococci. In the latest classification (2018) none were classified as Poor, with most being Excellent or Good.

Healthy and biologically diverse

This section summarises the information from the Marine Protected Areas (MPAs) and intertidal and continental shelf habitats assessments from SMA2020. It also provides information from the relevant case studies relating to Priority Marine Features (PMFs), with a focus on habitats.  Further work is required to enable assessment at a regional scale for most species; this will be included in Scotland’s next marine assessment.

At a regional scale for MPAs the focus is on the number of new MPAs, MPAs with new spatial management measures, and MPAs in which spatial management measures are in discussion, as well as recognising monitoring that has been undertaken between 2012-2018.  For the marine habitats, the focus is on interpreting the relevant intertidal and continental shelf habitat assessments – biogenic habitats, predicted extent of physical disturbance to the sea floor (BH3) and intertidal seagrass beds.  For PMFs, a summary is provided of the changes in our understanding of the habitats of most relevance to the North East SMR, including changes in distribution and extent.

Marine Protected Areas

Progress in developing the Scottish MPA network

There are five MPAs in the North East SMR that contribute to the Scottish MPA network (see Table 1).  Some of these MPAs overlap completely or partially in terms of their spatial coverage and/or the features (habitats, species, etc.) they were set up to help conserve.  They are counted as separate MPAs because they have been established under different legislation which influences the way in which they are managed.  Also note that there are MPAs that straddle the boundaries between different SMRs.  Where this is the case, these MPAs have been counted as contributing to the MPA network in all of the SMRs/OMRs in which they are present.  This means that the total number of MPAs in Scotland cannot be calculated through combining the regional totals.  Please see the Marine Protected Area assessment which contains statistics for the Scottish MPA network as a whole.  

Table 1. Numbers of types of MPAs in the North East SMR that contribute to the Scottish MPA network, including the number of new MPAs introduced since 2012.

Type of MPA

Abbr.

Total no. of MPAs

No. of new MPAs 2012-2018

Site of Special Scientific Interest

SSSI

1

0

Ramsar

-

1

0

Special Protection Area

SPA

3

0

Note that in December 2020 there was another one MPA designated in this region in addition to those in the table above (i.e. Southern Trench) as well as  an extension to an existing SPA (now known as Ythan Estuary, Sands of Forvie and Meikle Loch).

The various MPAs are focused on the protection of marine birds and their supporting habitats.  The existing Ythan Estuary, Sands of Forvie and Meikle Loch SPA supports internationally important numbers of wintering waterfowl and breeding populations of common, Sandwich and little terns. The recent extension of the SPA into the marine environment provides further protection for the foraging areas that Sandwich and little terns depend upon. Common redshank (and lapwing) are also now included as part of the waterbird assemblage within the existing SPA.  The Southern Trench MPA takes its name from the 58 km long, 9 km wide and 250 m deep trench running parallel to the Moray coast that was carved out by glaciers. Although the trench is located mainly within the Moray Firth SMR, the MPA extends into the northern part of the North East SMR.  Minke whale and an oceanic front are protected by this MPA.  The East Coast of Scotland is an Other Area Based Measure covering an area of 21,320 km2 to help conserve black-legged kittiwakes through protecting their main prey species, sandeels. 



Progress in managing MPAs

The progress in implementing management for MPAs in the North East SMR is summarised in Table 2.  This includes information on where spatial management measures are in place and where they are under discussion.  It also includes information on the number of MPAs that have been monitored, whether by statutory bodies or through citizen science.

Table 2. Summary of progress in managing Marine Protected Areas in the North East SMR. Note that the spatial measures listed in the table are in addition to the protection provided as a result of consideration of activities/developments through licensing and consenting processes.

Type of MPA

Spatial measures in place pre-2012

Spatial measures in place 2012-2018

Spatial  measures in discussion 2012-2018

No. of MPAs monitored by statutory bodies 2012-2018

No. of MPAs monitored via citizen science 2012-2018

Ramsar

0

0

0

1

0

Site of Special Scientific Interest

0

0

0

Birds

 

1

Birds

0

Special Protection Area

0

0

0

3

0

               

During this assessment period all of the MPAs have been monitored at least once by the statutory bodies, whether directly or through contracts, e.g. with the RSPB.  Monitoring has covered seabirds, and wintering waterbirds. 

Information on MPA boundaries can be viewed in Marine Scotland’s NMPi. To find out more about specific MPAs, please visit NatureScot’s SiteLINK.  Detailed reports on habitat monitoring are referenced in Further reading – seabed habitat monitoring reports.

Intertidal and continental shelf habitats

SMA2020 contains three relevant habitat assessments: intertidal seagrass beds, subtidal biogenic habitats, and predicted extent of physical disturbance to the seafloor.  Assessment of the status of subtidal biogenic habitats is based on temporal reductions in extent of six habitat types: seagrass beds, serpulid aggregations, flame shell beds, maerl beds, and horse and blue mussel beds.  None of these habitats have been recorded in the SMR and so no status assessment could be made.  There is also no known occurence of intertidal seagrass in the region.  Modelling work was carried out as part of the third assessment to predict the extent of physical disturbance to the seafloor more generally.

Predicted physical disturbance to the seafloor

To assess physical disturbance to seafloor habitats SMA2020 employed a modelling approach which generates a map of predicted relative disturbance levels from demersal fishing activity on a scale of 0 (zero) to 9 (severe).  The map was produced by the combination of information on the distribution of habitats, the sensitivity of the habitats (and species present to varying degrees) and the fishing pressure from demersal trawling, dredging and seine netting.  Fishing pressure information was derived from Vessel Monitoring System (VMS) data from 2012 - 2016 and was categorised as either surface abrasion (disturbance of surface and upper layers of sediment) or sub-surface abrasion (disturbance to a depth of >3 cm).  The final predicted disturbance index utilises the greater of these two pressure values and for descriptive purposes has been categorised as no disturbance (0), low disturbance (1-4) and high disturbance (5-9).

It should be emphasised that this method does not measure disturbance to seabed habitats, but predicts relative levels of disturbance. These relative levels are dependent upon the accuracy of habitat data and sensitivity assessments.  Many of the habitat data are derived from modelling and there is a low level of confidence in its accuracy.  Geographical variation in the accuracy of the sensitivity information employed is likely to be great, being dependent upon the level and quality of information used locally.  A significant limitation of the method is that during the assessment period pressure data were only available for vessels >12 m, which has probably resulted in an underestimation of disturbance for the SMRs.

Predicted habitat disturbance by mobile demersal fishing for the North East SMR is average for SMRs in terms of the proportion of the seabed, with 51% high disturbance compared to an average of 50% for all SMRs (Figure 3).  Five per cent of the seabed is predicted to experience no disturbance (average of 12% for all SMRs).  There are three fairly distinct areas showing the highest predicted disturbance levels – from Fraserburgh to Buchan Ness, and areas north east of Aberdeen and south east of Stonehaven.  This very much reflects the distribution of coarse sediments, the sensitivity of the benthic community to surface abrasion, and the surface and subsurface abrasion pressure.

Figure 3  Predicted physical disturbance to the seafloor in the North East SMR and prohibition areas for all mobile demersal fishing.

Priority Marine Features and birds (non-PMF)

Overview of recorded PMFs and birds

The North East SMR supports a range of PMFs and breeding seabirds as well as wintering waterbirds (i.e. waders, estuarine waterfowl, seaduck and coastal water feeding birds) as detailed in Table 3. 

Table 3: Details of PMFs, seabirds, and wintering waterbirds found in the North East SMR

Priority Marine Features (PMFs; grouped habitats and species) and birds

No. of species/

habitats recorded

Intertidal and continental shelf habitats

3

Fish[1]

21

Mammals (regularly occurring)

11

Shellfish & other invertebrates

2

Seabirds[2] (non-PMF) – breeding

17

Wintering waterbirds[3] (non-PMF) – non-breeding

14

There are 37 PMFs and 31 marine birds recorded in this SMR, which is relatively low compared to other marine regions.  This SMR overlaps with an important herring spawning area and supports the Scottish east coast bottlenose dolphin population, with easily accessible popular watching sites, including just outside Aberdeen Harbour.  Sandbanks at the mouth of the Ythan provide an important haulout and pupping site for grey seals.  

Progress in understanding of intertidal and continental shelf habitats listed as PMFs

The temporal sequence of records of all PMF habitats is provided in Table 4, based on inclusion in the Marine Recorder (2021) and GeMS (2021) databases, as well as identified additional sources.  Associated commentary, however, is restricted to PMFs for which the information has the potential to inform regional marine planning.  For example, some PMFs are excluded on the basis that they are very widely distributed and for which the records represent a small proportion of their likely distribution, such as several of the kelp habitats.  The geographical distribution of records of selected PMFs is shown in Figure 4.

Prior to 2012 very little survey work was carried out within the region that would facilitate the identification of PMFs.  Most of the relevant surveys were carried out by Seasearch divers, who focused on recording kelp beds.  There are no records of intertidal mudflats or mussel beds in either the Marine Recorder or GeMS databases, although both habitats are known to be present in the Ythan Estuary and have been described by Trewin (1986), Trewin & Welsh (1976) and Anderson (1971), the latter author having mapped the mudflats.

Since 2012 there have been a small number of localised surveys by Marine Scotland, SNH and JNCC with the main goal of identifying habitats and species of conservation importance (reported in Moore, 2015; 2019), although they have not increased the knowledge of PMF habitats in the region.  

Table 4.  Temporal frequency of PMF habitat records within the North East SMR obtained from GeMS (2021), Marine Recorder (2021) and other sources.  The numbers of All records are given, as well as those from Citizen Science (CS) surveys alone.

PMF

<2012

2012-2018

>2018

 

All

CS

All

CS

All

CS

Blue mussel beds (intertidal)

1

0

0

0

0

0

Burrowed mud

1

0

0

0

0

0

Intertidal mudflats

1

0

0

0

0

0

Kelp beds

4

4

1

1

0

0

Tide-swept algal communities

0

0

1

1

0

0

 

 

Figure 4.  Temporal pattern of records of selected PMF habitats for the North East SMR.

Status and trend in grey and harbour seals

There are no major grey seal breeding sites in the North East SMR and as part of the East Scotland Seal Management Unit they are assessed as having few or no concerns.  In contrast while historically harbour seal numbers were never very high they have suffered a decline of around 95% since the early 2000s although since 2012 their numbers are little changed albeit at a reduced level and their status is assessed as ‘some concerns’. 


[1] Records from International Bottom Trawl Surveys from MSS.

[2] Records of seabirds during breeding season only, from BTO Bird Atlas.

[3] Records of birds during the non-breeding season, from the BTO Bird Atlas

Climate change

There is good evidence that climate change is driving changes in the physical, chemical and biological conditions of the marine environment but the current evidence-base limits the ability to draw conclusions at the scale of the individual marine regions, including North East SMR. This is a combination of the lack of comprehensive spatial coverage of key monitoring programmes, the relatively short time series, and the complex linkages of climate change impacts in the marine environment.

Increasing concentrations of atmospheric greenhouse gases have caused more energy to be trapped within the Earth’s atmosphere, land and ocean. Approximately 90% of this excess energy has been absorbed by the ocean, resulting in warming ocean temperatures (see Temperature assessment and Climate change Sea temperature assessment).

The increasing concentration of carbon dioxide, one of these greenhouse gases, has the additional consequence of driving a reduction in the pH of the ocean, a process known as ocean acidification (see Ocean acidification assessment and Climate change Ocean acidification assessment).

Mean sea level is rising due to increased contributions of freshwater from melting of land-based ice (glaciers and the polar ice sheets) and due to thermal expansion of water (see Sea level and tides assessment and Climate change Sea level assessment).

The warming temperatures also result in lower oxygen concentrations due to fact that warm water holds less oxygen and changes in stratification further influence oxygen concentrations (see Dissolved oxygen assessment and Climate change Dissolved oxygen assessment). Together with increased metabolic rates in organisms resulting in increased respiration, oxygen depletion has a severe impact on marine organisms due to the impact on metabolic processes.

These changes in the physical environment are also having an impact on marine life, such as changes to their metabolism, changes in seasonality and the timing of events in natural cycles, and changes in their distribution. These changes have consequences for the growth, survival and abundance of species, including those of commercial importance or critical to conservation objectives.

At present, most of these impacts are assessed at scales greater than marine regions. The Community Temperature Index combines species temperature affinity and their abundances. This index has the potential to inform how communities change due to climate change. An example of changes in the Community Temperature Index from bottom-living fishes can be found in the Fish section within Biological Impacts of Climate Change, where more information on other impacts in marine food webs can be found (such as seabirds and marine mammals) on large regional scales in Scottish waters.

Sea surface temperature in the North East SMR has increased since 1870 by 0.05 °C per decade on average.  The rate of increase has not been constant, and in the last 30 years (1988-2017), the change in temperature was +0.23 °C per decade.

Although the most comprehensive data set for carbonate chemistry in the waters around Scotland is from the Stonehaven ecosystem monitoring site, which is within the North East SMR from 2009 – 2014, no discernible trend in pH has been detected as the time series is so short (see Ocean acidification assessment and Climate change Ocean acidification assessment). However, there is an indication, in amongst the seasonal and year-to-year variability, of a possible reduction in pH during the time period monitored. Furthermore, there is some evidence of biological impacts, specifically of shell dissolution (See shell integrity case study)

Tide gauge records from around Scotland’s coast show a high degree of year-to-year change in coastal water levels (typically several centimetres). The long-term average mean sea level change in the North East SMR, as estimated from a historical climate model run (UKCP18), was 5 cm (likely range between 2 and 8 cm) higher in 2018 than the 1981-2000 average. For reference, the Scottish average is estimated to be 5 cm (likely range between 3 and 8 cm). By 2100, mean sea level in the North East SMR is anticipated to be approximately 37 cm for a medium emissions scenario (UKCP18 RCP4.5; see also and Climate change Sea level assessment).

Detecting and understanding long-term change in biological time series is complex, and resolving that which is due to climate change remains a challenge. Data from the Continuous Plankton Recorder have shown a significant positive trend in the North East SMR for the plankton life forms: diatoms, pelagic diatoms and large copepods over the period 1980 – 2017 (see Plankton Assessment). Changes in diatoms show a correlation with sea surface temperature change. Data from the Scottish Coastal Observatory site at Stonehaven cover a shorter period (1999-2017) and show no significant trend for any plankton life forms.

Offshore renewable energy is an important component in respect of reducing emissions of greenhouse gases.  In 2018 the total installed wind capacity in the North East SMR was 95.2 MW.

Summary

The North East SMR contains the largest white fish market and port and the main port for the North Sea oil and gas industry.  A total (demersal, pelagic and shellfish) of 170,227 tonnes was landed into Peterhead and other small ports in the SMR in 2018. There has been an 6% decrease in freight tonnage and a 1% decrease in passenger numbers over the five years between 2014-2018.  Marine tourism and recreation declined with a 3% decrease in GVA in the four years between 2014-2017.  Dredge spoil disposal increased by 659% in the five years between 2014-2018.  Other active sectors include renewables, military activity, and subsea cables.

The five main pressures affecting the SMR are Removal of target species, Removal of non-target species, Physical change, Surface / Sub-surface abrasion / penetration, and Underwater noise.  Other active pressures identified are Introduction of non-indigenous species and Litter.

Nutrient inputs to the North East SMR are some of the highest of any SMR although there is no evidence of eutrophication in this SMR. Contaminant (i.e. PAHs, PCBs, PBDEs and heavy metals) concentrations are generally above background but below levels that might cause adverse biological effects.  There is an increasing trend in mercury inputs.  In some years there was evidence of an increase in fish disease but this could not be linked to exposure to contaminants.  Litter and microplastics are present with some evidence of an improving situation in relation to beach conditions.  There are few noise data, but noise levels are expected to rise as wind farm developments progress.  No bathing waters were classified as Poor, with most being Excellent or Good.

Fifty-one per cent of the seafloor is predicted to have been subject to high physical disturbance and 5% subject to none.  There are few records of benthic habitats in this SMR.

In the last 30 years sea temperature has risen by 0.23 °C per decade.  Sea level in 2018 is estimated 5cm higher than the 1981-2000 average.