Figure - available from: Ecological Applications
This content is subject to copyright. Terms and conditions apply.
(A) Location of sampled estuaries (red dots) and satellite aerial images of Saccostrea glomerata reef complexes along coastline of New South Wales (inset), Australia, where oyster recruitment was determined. (B) Hunter River. (C) Hawkesbury River. (D) Georges River. (E) Port Hacking. (F) Crookhaven River. (G) Bermagui River. Aerial images (B–F) and (G) were obtained from NearMap Ltd. (https://www.nearmap.com/au/en) and NSW Government Spatial Services (https://maps.six.nsw.gov.au/), respectively.

(A) Location of sampled estuaries (red dots) and satellite aerial images of Saccostrea glomerata reef complexes along coastline of New South Wales (inset), Australia, where oyster recruitment was determined. (B) Hunter River. (C) Hawkesbury River. (D) Georges River. (E) Port Hacking. (F) Crookhaven River. (G) Bermagui River. Aerial images (B–F) and (G) were obtained from NearMap Ltd. (https://www.nearmap.com/au/en) and NSW Government Spatial Services (https://maps.six.nsw.gov.au/), respectively.

Source publication
Article
Full-text available
Understanding how habitat attributes (e.g., patch area and sizes, connectivity) control recruitment and how this is modified by processes operating at larger spatial scales is fundamental to understanding population sustainability and developing successful long‐term restoration strategies for marine foundation species—including for globally threate...

Similar publications

Preprint
Full-text available
Several climate-driven processes take place in the Arctic fjords. These include ice-ocean interactions, changes in biodiversity and ocean circulation patterns, as well as coastal erosion phenomena. Conducting long-term oceanographic monitoring in the Arctic fjords is, therefore, essential for better understanding and predicting global environmental...