Bruce G . Hatcher | Cape Breton University (original) (raw)
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Papers by Bruce G . Hatcher
Oceanographic Literature Review, 1995
Biogeosciences, Sep 5, 2019
Environmental Biology of Fishes, Jul 30, 2018
Biological Conservation, Sep 1, 2018
Conservation Physiology, 2016
Conservation Physiology, 2019
Coral Reefs, Apr 1, 2004
... tropical coastal management. UNESCO, Paris Hatcher BG (2001) A framework for the classificati... more ... tropical coastal management. UNESCO, Paris Hatcher BG (2001) A framework for the classification of benthic communities of the Scotian Shelf for the maintenance of the diversity of the marine ecosystem. Final Report to Fish ...
Trends in Ecology and Evolution, May 1, 1988
Comparative Biochemistry and Physiology Part C: Comparative Pharmacology, 1988
Journal of the Fisheries Research Board of Canada, 1975
In Petpeswick Inlet, Nova Scotia, the above-ground portion of Spartina alterniflora lost an estim... more In Petpeswick Inlet, Nova Scotia, the above-ground portion of Spartina alterniflora lost an estimated 152 g dry weight m−2 of dead leaves during the growing season and reached an average biomass of 558 g dry weight m−2 at the end of the growing season. The total production of 710 g dry weight is higher than that recorded at many sites between Nova Scotia and North Carolina, in spite of the fact that in Nova Scotia the species is near the northern end of its range.
Marine Geology, Nov 1, 1993
Marine Geology, Mar 1, 1993
ABSTRACT Late Quaternary coral reefs have developed on the southwestern Australian margin, which ... more ABSTRACT Late Quaternary coral reefs have developed on the southwestern Australian margin, which has otherwise been characterised by cool-water carbonates since the Eocene. The Houtman Abrolhos coral reefs are at the limits of existence, extending, with the assistance of the Leeuwin Current, a poleward-flowing, warm water stream, into a region dominated by more temperate communities. Coring in the Easter Group reefs, supported by high precision dating, by both TIMS and 14C methods, has shown vigorous coral growth, with reefs over 26 m thick in the Holocene and over 15 m thick in the Last Interglacial. Each of the three Abrolhos platforms consists of a central platform composed of Last Interglacial reefs, about which windward and leeward Holocene reefs developed asymmetrically. Reef, peritidal and eolian facies comprise the emergent Last Interglacial limestones which are extensively calcretized, with reef facies up to 5 m above MSL. The Last Interglacial high stand lasted for at least 10 ka from 130 to 120 ka, and possibly 15 ka, from 132 to 117 ka. Holocene reef facies are also emergent by 0.5 m, and are overlain by peritidal and storm ridge facies in an upward-shallowing sequence. Windward (10 m thick) and leeward (26 m thick) Holocene reefs in the Easter Group show contrasting lithofacies. The wave-exposed windward reefs consist of a slow-growing association of coralline algal bindstones and coral framestones, whereas fast-growing coral framestones dominate the more protected leeward reefs. The leeward reefs commenced growth 10,000 years ago and grew to the present sea level by 6500 years ago, generating Holocene constructional topography consisting of ‘blue-hole’ terrain in the leeward parts of the platforms.
Oceanographic Literature Review, 1995
Biogeosciences, Sep 5, 2019
Environmental Biology of Fishes, Jul 30, 2018
Biological Conservation, Sep 1, 2018
Conservation Physiology, 2016
Conservation Physiology, 2019
Coral Reefs, Apr 1, 2004
... tropical coastal management. UNESCO, Paris Hatcher BG (2001) A framework for the classificati... more ... tropical coastal management. UNESCO, Paris Hatcher BG (2001) A framework for the classification of benthic communities of the Scotian Shelf for the maintenance of the diversity of the marine ecosystem. Final Report to Fish ...
Trends in Ecology and Evolution, May 1, 1988
Comparative Biochemistry and Physiology Part C: Comparative Pharmacology, 1988
Journal of the Fisheries Research Board of Canada, 1975
In Petpeswick Inlet, Nova Scotia, the above-ground portion of Spartina alterniflora lost an estim... more In Petpeswick Inlet, Nova Scotia, the above-ground portion of Spartina alterniflora lost an estimated 152 g dry weight m−2 of dead leaves during the growing season and reached an average biomass of 558 g dry weight m−2 at the end of the growing season. The total production of 710 g dry weight is higher than that recorded at many sites between Nova Scotia and North Carolina, in spite of the fact that in Nova Scotia the species is near the northern end of its range.
Marine Geology, Nov 1, 1993
Marine Geology, Mar 1, 1993
ABSTRACT Late Quaternary coral reefs have developed on the southwestern Australian margin, which ... more ABSTRACT Late Quaternary coral reefs have developed on the southwestern Australian margin, which has otherwise been characterised by cool-water carbonates since the Eocene. The Houtman Abrolhos coral reefs are at the limits of existence, extending, with the assistance of the Leeuwin Current, a poleward-flowing, warm water stream, into a region dominated by more temperate communities. Coring in the Easter Group reefs, supported by high precision dating, by both TIMS and 14C methods, has shown vigorous coral growth, with reefs over 26 m thick in the Holocene and over 15 m thick in the Last Interglacial. Each of the three Abrolhos platforms consists of a central platform composed of Last Interglacial reefs, about which windward and leeward Holocene reefs developed asymmetrically. Reef, peritidal and eolian facies comprise the emergent Last Interglacial limestones which are extensively calcretized, with reef facies up to 5 m above MSL. The Last Interglacial high stand lasted for at least 10 ka from 130 to 120 ka, and possibly 15 ka, from 132 to 117 ka. Holocene reef facies are also emergent by 0.5 m, and are overlain by peritidal and storm ridge facies in an upward-shallowing sequence. Windward (10 m thick) and leeward (26 m thick) Holocene reefs in the Easter Group show contrasting lithofacies. The wave-exposed windward reefs consist of a slow-growing association of coralline algal bindstones and coral framestones, whereas fast-growing coral framestones dominate the more protected leeward reefs. The leeward reefs commenced growth 10,000 years ago and grew to the present sea level by 6500 years ago, generating Holocene constructional topography consisting of ‘blue-hole’ terrain in the leeward parts of the platforms.