Rob's lectures Flashcards
(52 cards)
Distribution patters influenced by environmental gradients
1.Particle size (grain size gradient)
2.Salinity
3.Vertical (emersion, depth)
4.Wave exposure
5.Latitude + temperature
6.Anthropogenic disturbance
1 particle size
-Muddy shores (mangroves)- terrestrial plants, halophyte (salt tolerant), anoxic sediments (adaptation), sediment accretion, coastal erosion and protection. Infaunal communities. Serve as sponges for refuge for other species, they also buffer and absorb storms for us.
-Sandy beaches- physical substrate shifts and is unstable. Burrow to avoid stress and predation, substrate disturbance from waves, fauna rely on imported food. Low primary production.
-Stones + boulders- intermediate disturbance hypothesis, disturbed habitats can have more diversity than undisturbed/pristine habitats.
-Rocky shore- hard and stable substrate, organisms are visible. Live on top of substrate as epifauna and epifloral. Tend to be abundant and small, or sessile and sedentary.
2 salinity gradients
-catchment to coast. Fully marine = 35 psu/ppt. Can be fully stratified, moderately stratified (tide mixing or wind), vertically homogenous.
-estuaries- variable salinity regime with few true estuarine species (that complete the whole cycle. Many visitors; both anadromous, catadromous. Adaptations include Osmoconforming and osmoregulation.
-rivers- broader biogeographic impacts of freshwater input. Yangtze river plume has been going on for years and speciation is occurring now.
3 Vertical- shallow subtidal to intertidal terrestrial
Ecotones = abrupt changes in vegetation or two adjacent and homogenous community types, producing a narrow ecological zone between them. Zonation also within coral reefs (also in forests).
4 wave exposure gradients
Horizontal along shore line. If waves change the coastline, the coastline changes the biodiversity.
6 anthropogenic disturbance gradient
There is normally a functional homogenization. Artificialisation of coastline.
Upwelling
Driven by surface winds, either seasonal or constant. Normally drags water up from the bottom and pushes warm surface water down.
Aragonite
A crystal form of calcium carbonate, which is the primary mineral used by corals to build their skeleton. It’s more soluble than calcite so it dissolves more in acidic waters. It forms coral reefs; they extract calcium and carbonate from seawater to make the aragonite.
Aragonite saturation State (Ωₐ )
-Ωₐ > 3.3 → Favourable for coral growth.
-Ωₐ ~2.5 → Growth slows, dissolution increases.
-Ωₐ < 2.0 → Corals struggle to grow, reef erosion outpaces growth.
Natural acidification in Bahía Culebra
-Seasonal upwelling bring carbon dioxide rich waters and low pH waters
-Non-upwelling seasons still see acidification events
-Daily or seasonal fluctuations are controlled by photosynthesis and offshore water input
Aragonite saturation (Ωₐ): upwelling vs none
-Non-upwelling: Ωₐ > 3.3
-Upwelling: Ωₐ < 2.5 (reduced calcification & increased dissolution).
Coral growth in low pH
Showed high coral extension rates despite natural acidification. When the conditions aren’t right their growth slows, but then when the conditions are right, they grow even faster. But reefs are really thin despite how they are spread out. This may be because there is high bio-erosion and dissolution, which prevents long-term reef accumulation since it’s hollowing out from the bottom.
Red tides
Pollution when there is a lot of shit in the sea. Normally with heavy rains and strong upwelling.
Succession
The non-seasonal, directional + continuous pattern of colonisation + extinction of species populations.
Primary succession
Succession in an area where no organisms are present. For example, if artificial pontoons are introduced and algae starts growing on it.
Secondary succession
Succession in an area where a biological community is partially intact. Like extreme wave exposure on a rocky shore.
Degradative succession
Succession on or in dead or dying organic matter.
1883 eruption of Krakatoa
70% of island was blown out, including jungle, animals, humans. It put so much ash in the atmosphere that the earth actually cooled. It was the first time Europeans started studying succession. However, nature came back over time.
The climax state: differing hypothesis
An emergent stable community in a successional series is called the climax state, which is self-perpetuating and in equilibrium with the physical and biotic environment.
-Monoclimax hypothesis = only one climax community toward which all communities are developing
-Polyclimax hypothesis = many climax communities may be recognised in an area
-Climax-pattern hypothesis = natural communities are adapted to the environmental factors.
Regime shifts
Or phase shifts
-When the ecosystem state shifts due to an environmental driver
-Also known as alternative stable states
Coral reefs
-Non-reef building is called ahermatypic, globally distributed
-Reef-building is called hermatypic, but are mainly restricted to the tropics. They live in colonies, skeletons deposit CaCO3, polyps have zooxanthellae, and do photosynthesis by day and feed with nematocysts by night.
Corals resource availability
coral have improved resource availability through the coral-polyp associations through obligate mutualism and trophic interactions. Zooxanthellae provide nutrition to the corals as photosynthate, and they get nitrogen as a coral waste product.
Coral landscapes of fear
-There are grazing halos which are made by the predator-prey interactions. Sharks push all of the grazers into limited patches around the reefs.
-Without predators there are no halos.
EU habitats directive definitions of a reef
Reefs can be either biogenic concretions or of geogenic origin. They are hard compact substrata on solid & soft bottoms, which arise from the sea floor in the sublittoral & littoral zone. Reefs may support a zonation of benthic communities of algae & animal species as well as concretions & corallogenic concretions.