Coral reef growth in an era of rapidly rising sea level: predictions and suggestions for long-term research

Coral Reefs ◽  
1988 ◽  
Vol 7 (1) ◽  
pp. 51-56 ◽  
Author(s):  
R. W. Buddemeier ◽  
S. V. Smith
Keyword(s):  
Coral Reef ◽  
Sea Level ◽  
Reef Growth ◽  
Rising Sea Level

scholarly journals Measuring Sound at a Cold-Water Coral Reef to Assess the Impact of COVID-19 on Noise Pollution

2021 ◽  
Vol 8 ◽  
Author(s):  
Laurence H. De Clippele ◽  
Denise Risch
Keyword(s):  
Coral Reef ◽  
Coral Reefs ◽  
Sea Level ◽  
Cold Water ◽  
Noise Pollution ◽  
Ecosystem Functions ◽  
Noise Levels ◽  
Level Height ◽  
Water Coral

This study compares the noise levels at the cold-water coral Tisler reef, before and after the closure of the border between Norway and Sweden, which occurred as a direct result of the COVID-19 pandemic. The Tisler reef is a marine protected area located under a ferry “highway” that connects Norway and Sweden. Cold-water coral reefs are recognised as being important hotspots of both biodiversity and biomass, they function as breeding and nursing grounds for commercially important fish and are essential in providing ecosystem functions. Whilst studies have shown that fishery, ocean warming, and acidification threaten them, the effects of noise pollution on cold-water coral reefs remains unstudied. To study the severity of noise pollution at the Tisler reef, a long-term acoustic recorder was deployed from 29 January 2020 until 26 May 2020. From 15 March COVID-19 lockdown measures stopped passenger vessel traffic between Norway and Sweden. This study found that the overall noise levels were significantly lower after border closure, due to reduced ferry traffic, wind speeds, and sea level height. When comparing the median hourly noise levels of before vs. after border closure, this study measured a significant reduction in the 63–125 Hz 1/3 octave band noise levels of 8.94 ± 0.88 (MAD) dB during the day (07:00:00–19:59:59) and 1.94 ± 0.11 (MAD) dB during the night (20:00:00–06:59:59). Since there was no ferry traffic during the night, the drop in noise levels at night was likely driven by seasonal changes, i.e., the reduction in wind speed and sea level height when transitioning from winter to spring. Taking into account this seasonal effect, it can be deduced that the COVID-19 border closure reduced the noise levels in the 63–125 Hz 1/3 octave bands at the Tisler reef by 7.0 ± 0.99 (MAD) dB during the day. While the contribution of, and changes in biological, weather-related and geophysical sound sources remain to be assessed in more detail, understanding the extent of anthropogenic noise pollution at the Tisler cold-water coral reef is critical to guide effective management to ensure the long-term health and conservation of its ecosystem functions.

scholarly journals Loss of coral reef growth capacity to track future increases in sea level

Nature ◽  
2018 ◽  
Vol 558 (7710) ◽  
pp. 396-400 ◽  
Author(s):  
Chris T. Perry ◽  
Lorenzo Alvarez-Filip ◽  
Nicholas A. J. Graham ◽  
Peter J. Mumby ◽  
Shaun K. Wilson ◽  
...  
Keyword(s):  
Coral Reef ◽  
Sea Level ◽  
Reef Growth ◽  
Growth Capacity

scholarly journals Role of Future Reef Growth on Morphological Response of Coral Reef Islands to Sea-Level Rise

2020 ◽  
Author(s):  
Gerhard Masselink ◽  
Robert McCall ◽  
Edward Beetham ◽  
Paul Simon Kench ◽  
Curt D. Storlazzi
Keyword(s):  
Coral Reef ◽  
Sea Level Rise ◽  
Sea Level ◽  
Reef Growth ◽  
Morphological Response ◽  
Reef Islands

scholarly journals Role of Future Reef Growth on Morphological Response of Coral Reef Islands to Sea‐Level Rise

2021 ◽  
Vol 126 (2) ◽  
Author(s):  
G. Masselink ◽  
R. McCall ◽  
E. Beetham ◽  
P. Kench ◽  
C. Storlazzi
Keyword(s):  
Coral Reef ◽  
Sea Level Rise ◽  
Sea Level ◽  
Reef Growth ◽  
Morphological Response ◽  
Reef Islands

scholarly journals Short-Term Sea Level Changes of the Upper Cretaceous Carbonates: Calibration between Palynomorphs Composition, Inorganic Geochemistry, and Stable Isotopes

Minerals ◽  
2020 ◽  
Vol 10 (12) ◽  
pp. 1099
Author(s):  
Ahmed Mansour ◽  
Thomas Gentzis ◽  
Michael Wagreich ◽  
Sameh S. Tahoun ◽  
Ashraf M.T. Elewa
Keyword(s):  
Sea Level ◽  
Late Cretaceous ◽  
Upper Cretaceous ◽  
Freshwater Algae ◽  
Sea Level Changes ◽  
Short Term ◽  
Sea Level Oscillations ◽  
Rising Sea Level ◽  
Southern Tethys

Widespread deposition of pelagic-hemipelagic sediments provide an archive for the Late Cretaceous greenhouse that triggered sea level oscillations. Global distribution of dinoflagellate cysts (dinocysts) exhibited a comparable pattern to the eustatic sea level, and thus, considered reliable indicators for sea level and sequence stratigraphic reconstructions. Highly diverse assemblage of marine palynomorphs along with elemental proxies that relate to carbonates and siliciclastics and bulk carbonate δ13C and δ18O from the Upper Cretaceous Abu Roash A Member were used to reconstruct short-term sea level oscillations in the Abu Gharadig Basin, southern Tethys. Additionally, we investigated the relationship between various palynological, elemental, and isotope geochemistry parameters and their response to sea level changes and examined the link between these sea level changes and Late Cretaceous climate. This multiproxy approach revealed that a long-term sea-level rise, interrupted by minor short-term fall, was prevalent during the Coniacian-earliest Campanian in the southern Tethys, which allowed to divide the studied succession into four complete and two incomplete 3rd order transgressive-regressive sequences. Carbon and oxygen isotopes of bulk hemipelagic carbonates were calibrated with gonyaulacoids and freshwater algae (FWA)-pteridophyte spores and results showed that positive δ13Ccarb trends were consistent, in part, with excess gonyaulacoid dinocysts and reduced FWA-spores, reinforcing a rising sea level and vice versa. A reverse pattern was shown between the δ18Ocarb and gonyaulacoid dinocysts, where negative δ18Ocarb trends were slightly consistent with enhanced gonyaulacoid content, indicating a rising sea level and vice versa. However, stable isotope trends were not in agreement with palynological calibrations at some intervals. Therefore, the isotope records can be used as reliable indicators for reconstructing changes in long-term sea level rather than short-term oscillations.

Calcium Carbonate Production, Coral Reef Growth, and Sea Level Change

Science ◽  
1976 ◽  
Vol 194 (4268) ◽  
pp. 937-939 ◽  
Author(s):  
S. V. SMITH ◽  
D. W. KINSEY
Keyword(s):  
Coral Reef ◽  
Calcium Carbonate ◽  
Sea Level ◽  
Sea Level Change ◽  
Reef Growth ◽  
Carbonate Production ◽  
Level Change ◽  
And Sea Level

scholarly journals Ordovician reef and mound evolution: the Baltoscandian picture

2016 ◽  
Vol 154 (4) ◽  
pp. 683-706 ◽  
Author(s):  
BJÖRN KRÖGER ◽  
LINDA HINTS ◽  
OLIVER LEHNERT
Keyword(s):  
Sea Level ◽  
Climatic Conditions ◽  
Late Ordovician ◽  
Reef Growth ◽  
Baltic Basin ◽  
Reef Development ◽  
The Baltic ◽  
Oceanographic Conditions ◽  
Main Factor

AbstractThe widespread growth of reefs formed by a framework of biogenic constructors and frame-lacking carbonate mounds began on Baltica during Ordovician time. Previously, Ordovician reef and mound development on Baltica was considered to be sporadic and local. A review of all known bioherm localities across the Baltic Basin reveals a more consistent pattern. Ordovician bioherms grew in a wide E–W-aligned belt across the Baltic Basin and occur in several places in Norway. Substantial reef development began simultaneously across the region during the late Sandbian – early Katian interval and climaxed during the late Katian Pirgu age. The current spatiotemporal distribution of bioherms is a result of interdependent factors that involve original drivers of reef development such as relative sea level, climate during the time of deposition and effects of post-depositional erosion. Oceanographic conditions were likely more favourable during times of cooler global climates, low sea level and glacial episodes. At the same time, the likelihood that bioherms are preserved from long-term erosion is higher when deposited during low sea level in deeper parts of the basin. A main factor controlling the timing of the reef and mound evolution was Baltica's shift toward palaeotropical latitudes during Late Ordovician time. The time equivalence between initial reef growth and the Guttenberg isotope carbon excursion (GICE) suggests that global climatic conditions were important.

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