目前NOAA更新了墨西哥灣的各項資訊並製作成圖。可以在以下的連結中, 選擇欲覽類別, 可有生物環境, 魚類遷徙, 植物分布, 生態區位狀態。基本的地形預覽, 格局, 空照/簡單色彩也可以選擇。

我找了土地利用與生態系統分布圖~

LA土地利用與生態系統    

 

這張圖顯示出海岸以Palustrine Emergent Wetland (淺螢光粉紅)Estuarine Emergent wetland (紫粉紅) 為主, 內陸在Mississippi River附近的棕色部份, 表示cultivated land, 這些地區則以各項農業開發為主, 主要產出包括玉米, 甘蔗,... 等。

Palustrine  指的是
All nontidal wetlands dominated by trees, shrubs, persistent emergents, emergent mosses, or lichens, and all such wetlands that occur in tidal areas where salinity stemming from ocean-derived salts is below 0.5ppt (0.5 mg salt in 1 L water, considered as freshwater). 

It also includes wetlands lacking such vegetation but with all of the following characteristics: 
1) areas less than 8ha
2) lack of active water-formed or bedrock shoreline features
3) Water depth in the deepest part of the basin of less than 2 m at low water
4) salinity stemming from ocean-derived salts of less than 0.5 ppt.  

Estuarine 指的是
Deepwater tidal habitats and adjacent tidal wetlands that are usually semi-enclosed by land but have open, partially obstructed, or sporadic access to the ocean and in which ocean water is at least occasionally diluted by freshwater runoff from the land.  

 

Note that there is no Lacustrine here. Lacustrine is 
Wetlands and deepwater habitats with all of the following characteristics: 

1) situated in a topographic depression or a dammed river channel;
2) lacking trees, shrubs, persistent emergents, emergent mosses, or lichens with greater than 30% areal coverage
3) total area in excess of 8 ha.
Similar wetland and deepwater habitats totaling less than 8ha are also included in the lacustrine system when an active water-formed or bedrock shoreline feature makes up all or part of the boundary or when the depth in the deepest part of the basin exceeds 2 m at low water.  

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Environmental Chemodynamics

This topic is about knowing how chemicals movement in the environment. We predict it pathway and rate of change according to the chemical potential and weather condition in between phases. It involves chemical concentration changes during equilibrium, diffusion, transportation processes near natural phases and boundary regions. It's a way to predict the fate of anthropogenic substances in which we quantify the phase distribution fractions, flux rates, reaction rates, half-lives, and concentration levels. 

First fundemental is "Mass balance" 
There is no gain or lose of matter during the course of chemical and phases transformation. The fate of a chemical consists with chemical mobility, partitioning, dissipation rate, concentration level, residence time etc in between phases. 
 EX. Stream assimilation capacity,  

Second fundemental is "Chemical equilibrium" 

Third fundemental is "Mass transfer" 

 

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1)      Define geomorphology.  What is the role of geomorphology in structuring floodplain ecosystems? 

 

Geomorphology is about hownatural or non-natural processes transform the shapeand characters of the landscape. Above all, endogenic factor includes properties of rocks and also soil; exogenic factor includes formation processes, such as weathering, transportation, and erosion. Specifically in a river system, active hydrological force plays a major part in geomorphologic processes. Hence, factors like tectonic (relief), lithology (soil), climate (hydrology), river history, and human are important geomorphologic forces in structuring a fluvial system.  The geomorphology features also affect how vegetation establishes.

 

Tectonic force: Earthquake could also induce formation of a lake by land sink and river cutoff, i.e. Reelfoot Lake. The lake was formed during New Madrid earthquakes around 1811 in Tennessee, USA.

Lithology: Soil quality relates to particle structure and its stability. For example, mineral contains and soil texture relate to stability of weathering or erosion. Sizes of soil particle also control the sedimentation process. Small particles like clay could be transported further. Clay plug happens when flow transportation force is smaller than sedimentation; clay plug thus blocks meandering channels. Soil types affect vegetation establishment.

On the other hand, vegetation could reduce the erodibility of the land and increase sedimentation. For example, loess structure breaks down by water erosion or wind blow. Such erosion gets worse if vegetation is absent. This is also a prevalent problem in the upper Mississippi River Basin because most of the riverine areas were transformed into agricultural lands a hundred years ago, like what we saw in West Tennessee.

Climate: The geomorphologic change of a river comes from its geologic history as well as hydrological feature and sediment loads. A river could be abandoned by sedimentation and changed river course. Topographic change of a river system relates to hydrologic pattern. Overtopped flooding will induce further deposition of sediment away from river channel and thus forms ridge and swale.

River history: Mississippi River was with braided channels in the past but now become meandered ones. Because stream power increased with larger scouring force to the riverbed, flow focuses on a single channel.

Human:   From European settlement to present, urbanization, agricultural lands have removed vegetation cover. River control systems like levees, channelization, and dams have increased discharge quantity, stream power.


Overall, geomorphologic variance in a floodplain influences the topography, hydroperiod, and edaphic quality. Those features are favored by different group of vegetation. Vegetation groups and hydrologic connectivity change influence the availability of food resources to wildlife. Also, the variability affects wildlife migration and niches.  

 

 

2)     Define and explain hydrologic connectivity as it pertains to floodplain ecosystems. Discuss temporal and spatial variability in connectivity and associated ecological processes.   In what ways can hydrologic connectivity be disrupted?  What effects can disruption have on floodplain ecosystems? 

 

Hydrologic connectivity is about how water moves within a floodplain ecosystem. River connectivity changes with river stages and geomorphologic features. The change of river connectivity also affects ecological functions. For example, the height of the water level in growing season could define the chance of survival to plants.

 

For example, oxbows are cut off from river for a long time; higher river stage may also replenish nutrients to the river. Generally, oxbows are important habitats for fish. Ridge and swale are formed from point bar as stream migrates across the floodplain, the variance of topography and vicinity of water provides important habitat for birds, amphibians, and more animals. Turtles with different species, and sexes utilize the habitat with their own niches, i.e. Graptemys psudogeographica females and Trachemys scripta females and males mostly use in river while G. psudogeographica males prefer scours. Temporary changes of river stage affect the water levels. Plant species also have different tolerance to flooding. Baldcypress, water tupelo and water elm mostly occur in oxbows and water hickory, overcup oak, green ash, and red maple could be found in shallower area with less water flooding. As hydroperiod gets shorter and elevation gets higher, you will find out more Black gum, white oak, cherrybark oak, and water oak. 

 

Hydrological connectivity can be disrupted by human utilization, climate change, and channelization and also river structure.  If the rivers are channelized, stream power could be enhanced within narrower, shorter water path and essentially scouring down the riverbed. Consequently, nick point shifts upland and thus lower riverbed of upstream rivers. And again the level of groundwater in the upper stream basin will be lowered adjusting to the lowered riverbed. Upper stream wetlands thus degrade with few water source.

 

 

1)     You are in charge of stream restoration in western Tennessee for Tennessee Department of Environment and Conservation, and must design a comprehensive plan to address restoration issues.  Please outline and briefly explain your overall goals and objectives.  Also, please compare and contrast the restoration methods that we observed and discussed in West Tennessee including re-creating meandering streams (and their location in the watershed), purposely creating valley plugs in tributaries, and developing drop structures on streams. 

 

My priority is to set up focal areas. In Tennessee, the agricultural lands are inducing land erosion and increase channelization of the rivers. First, I will find areas with higher ecological instability, such as increased hydroperiod, stream power, and lose river connectivity and higher biodiversity loss as my target ecosystem restoration areas. But I understand that we will definitely be facing a lot of conflicts. So, secondly I only ask for 20% improvement in the health of our stream, forest, and wildlife.

 

The only thing to get rid of conflicts and get things going is to purchase target lands and also search cooperation with neighbor farmers.  We will try to bribe them in getting a wetland mitigation, EPA assistance on improving water quality, or agricultural improvement program.

 

As we saw how Jody did in Arkansas, we could apply similar method in producing such cooperation scheme. We will restore hydroperiod pattern of a Green tree reservoir with river water braided/ meandered amid the forest in winter. In spring, agricultural landowners could work on their desired crops. Plants are shown to have larger growth with abundant water and thus they provide enough food sources to fauna. Crop will be cut in the fall, where prairie land becomes inundated by river water. Inundation helps wildlife reproduction. Frequent inundation of soils could enhance fertilization for next spring. Meanwhile, forests remain dry in the growing season with more chances of seedling survival.

 

Here is my procedure,

Step1. Choose target area of restoration

èIdentifying the area with most rainfall.

èIdentifying areas with most stream power

èIdentifying areas with the worst channelization occurs

èIdentifying areas with diverse ecosystem

èThen yes, purchase them all or find ways to cooperate with landowners


Step 2. Implementing measures by severity

à Worst disturbed area such as valley plug, gully erosion, no generation of plants should be implement drop structures and bank stabilization methods in slowing the water velocity, stream power, and vegetation dying. (Case studies are applied from West Tennessee)

à Moderate problems on forests degradation with abandoned stream that lost connectivity from river or prolonged flooding problem.

à Restoring vegetation groups according to the Potential Natural Vegetation. In supplementary, we also induce native understory grass and shrubs. Because they could establish quickly in floodplain area, they are able to provide vegetation mat for woody trees, i.e. Swamp loosestrife (Dacodon verticillatus) in the Reelfoot Lake provides a living mat for the basement of baldcypress trees.

 

Step 3. Active responses to hydroperiod

à Increase the quantity of water absorption in the upper stream.

à Don’t manipulate the timing the flooding during growing season and be careful about the water level.  Because over manipulate will only decrease the original function of the ecosystem.

Step 4. Maintenance and monitoring

à Removal of aggressive invasive species: target species are water hyacinth or similar aquatic species. Because those species grow rapidly and seriously block the living space of the other native plants.

 

 

2)     Explain the Potential Vegetation Community concept by Klimas et al.  What were the major steps/data layers needed?  Give examples where this approach to classifying and managing floodplains would work or not work in other floodplain ecosystems and explain why or why not.

 

The PNV concept is to classify vegetation groups and match their natural occurrence with abiotic features. The reason is very straightforward. Plants follow abiotic features because every species could have their niches and living requirements like limitations of nutrients, water, or light. In this model, they use three factors, hydrology, geomorphology, and soil; and their target is the Mississippi floodplain.  

 

Steps

First, overall field sampling and classification. Then forest dominance type is divided into groups according to their geomorphic and hydrologic settings. Second, combine hydrology, geomorphology, and soils from the field. Seek out unique combinations of the three variables for which little or no vegetation sample data had been collected. Primary inputs to the PNV model were geomorphology, soils, and hydrology (flood frequency). The potential group will be mapped in the GIS map. The PNV will be examined over again with HGM classification protocols in the field.  

PNV concept may not work on other ecosystems. In yellow river of China, the major problems have been wind and water erosion, pollution, and urbanization. Hence, extra criteria should be taken into account.

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路州有三個河口, 密西西比河(Mississippi River), 阿契法拉雅河(Atchafalaya River), 與波爾河(Pearl River). 密河以流域面積著稱, 阿河以生物多樣度高著稱, 波爾河則是密河堤岸後的流域, 不與密河相接。

先來介紹阿河流域:阿河為密河與紅河(Red River)的合流之後的, 再分出來的支流。 目前下游一百英里()周邊圍起提防作為大型的密河流域盆地, 為的是減低密河的出水量。所以自紐澳良出海的河口已經很少了。

marb_pop1.cfm.jpg

 

marb5

Basin Area:

  • The basin covers more than 1,245,000 square miles
  • 41% of contiguous United States
  • 15% of North America
  • First began to form around 900 AD when the ancient M. River moved from one channel to another. 
  • At one time, Bayou Teche is believed to have been the natural course of the M. River and from there made its way east to its present course. This is believed to have taken some 3000 years. 

Size of River:

  • The Mississippi River runs 2,350 miles (3,781 km) from its headwaters at Lake Itasca, Minnesota to the mouth of the Gulf of Mexico
  • The width of the Mississippi ranges from 20 feet at the headwaters, to about 1 mile across in Louisiana

Water Discharge Rate:

  • Water is discharged into the Gulf of Mexico at an average rate of 600,000 cubic feet per second
  • It takes about 90 days for water to travel from the headwaters in Minnesota to the Gulf of Mexico
  • 5 times more productive than any other river basin in the North America. 

Wildlife Facts:

  • 260 fish species
  • 145 amphibians and reptiles
  • 50 mammals
  • 38 mussel species
  • 60% of North American birds use the Mississippi River as their migratory flyway
  • Over 250 known species of birds in Atchafalaya Basin, including American Bald Eagle, ivory-billed woodpecker (now extinct?), Bachman's warbler, the peregrine falcon. 
  • Other species include: Florida panther, black bear, bobcat, nutria, mink, fox, muskrat, beaver, otter, raccoon, and others. 
  • The largest nesting concentration of bald eagles in the south central US is found in Atchafalaya basin. 
  • The Black Bear Wildlife Refuge in Franklin La. is home to the largest concentration of Louisiana Black Bears in North America. 
  • The basin contains the largest contiguous bottomland hardwood forest in North America and is the largest overflow alluvial hardwood swamp remaining in the US.  

Other Facts:

  • 60% of grain exported from the United States is transported and shipped from the Mississippi River
  • The Mississippi carries an average of 436,000 tons of sediment each day
  • More than 50 cities rely on the Mississippi for daily water supply
  • The Port of South Louisiana, which stretches 54 miles along the Mississippi River, is the largest tonnage port district in the United States, moving some 233 million short tons of cargo in 2008.
  • Missouri's New Madrid earthquakes in 1811 and 1812 caused the Mississippi River to flow backwards
  • An estimated average annual commercial harvest of nearly 22 million pounds of crawfish. 

引用連結EPA

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Reducing human bear conflict

Our approach to reducing Human Bear Conflict is explored more fully in Principles of Human Bear Conflict reduction (WSPA, 2009), a document prepared by wildlife experts (including IUCN specialists) and social scientists to inform governments and specialised non-government organisations.

1. Managing conflict humanely: In summary

The Principles document advocates that governmental and non-governmental organisations looking to protect people and bears by addressing Human Bear Conflict (HBC) humanely and effectively should take the following steps:

  • 辨釋與物種衝突的狀態, 範圍,地點 Identify the specific nature, extent and location of the conflict situations. Scientifically informed conflict management actions can reduce the frequency and intensity of HBC. 
  • 針對各個機關的需求與期待, 在人類容許熊群減少量之前降低衝突 Identify and understand the differing perceptions, values, needs and demands of the stakeholders. Taking a proactive approach whenever possible helps to reduce conflict situations before human tolerance for bears declines. 
  • 大眾參與與立法Gain public input and political will. Establishing local working groups with an effective decision making structure and access to resources, alongside participation and collaboration by essential stakeholders, can assist in building effective plans and implementing actions to reduce conflict.
  • Achieve stakeholder acceptance, cost-effectiveness and efficacy of proposed interventions. Conflict reduction methods that are familiar, inexpensive, require little new technology and minimal change to existing human behaviours are most likely to be adopted by local people.
  • 熊群與人的衝突狀況監測與分析Carry out monitoring and evaluation. A project’s parameters may change as bears react to the methods of reducing conflict. Long-term engagement and a willingness to adapt the project will offer a higher chance of addressing conflict situations effectively. 

Steps towards humane conflict reduction

Effective, long-term approaches require methods, techniques and tools that integrate the needs and behaviours of both humans and bears, and address the root causes of conflict:

Human-focused interventions

  • Education and awareness
  • Avoiding negative encounters
  • Removal of attractants
  • Direct compensation

Bear-focused interventions

  • Physical Barriers
  • Bear deterrents
  • Aversive behavioural conditioning
  • Bear population management
  • Habitat management
  • Removal of ‘nuisance bears’ from the conflict area

 

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"Now, a group of maverick ecologists is promoting the idea that the addition of nonnative species to natives in a region leads to "novel" or "hybrid" ecosystems that have ecological value and may be worthy of conservation." ... Gaia Vince, Science 18 March 2011

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Today we went to Bayou Cocodrie. This is really an awesome place! I got to see the unique old growth forest that had survived from the cutting 90 years ago. This bottomland hardwood forest just represents the diversity in many ways. The instructor John was doing a great job in combing all releam of studies applied in the ecosystem. 

The one thing I am sad about is that I didn't recharge my battery. 

Well, there are other people who got the cameras!^^ 

Sum up the info later... So tired!

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Sunny, 50-71F, 10:30a - 3:00pm. Cat Island National Wildlife Refuge Area, LA


檢視較大的地圖

"Oldest Baldcypress Tree in the US, 6th oldest."

 

Trail: Big cypress trail 0.5mi, Blackfork trail 3.6mi. 

Woody Plant species:

Water hickory (Carya aquatica),

Green Ash, Sugar berry, Water Elm, Overcup oak (Quercus lyrata), Nuttal Oak, Baldcypress, Water tupelo, Chinese Privite ... 

Crew: April, April Mason, Bred, Hugo, Ben, Nike, Ashby, Jill, a couple. 

Cat island P2136267.JPG 

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Interaction s between groundwater and surface water: the state of the science by Marios sophocleous

 

The topic is about related aspects for groundwater and surface water in which they are connected with ways which climate, landform, geology, and biotic factors are interplay.

 

This GW-SW relationship also applies to ecological impact. They  outline the mechanisms of GW-SW and point out the importance of sediments beneath the surface-water bodies --- the hyporheic zone.

 

Here is my note:

Introduction

(the topic arises when contaimination is serious around 60's. GW-SW interacts and co-developes along the time/spatial scale. Exchange water between near-channel and in-channel water is key to evaluate the ecological  structure of stream systems)

 

Principal geomorphologic, hydrogeologic, and climatic controls on groundwater flow systems and GW-SW interactions

Hydrological environment of groundwater flow system is the effects of topography, geology, and climate combined. Groundwater flows within a predicable pattern and is organized in space as a flow system. They define the spatial scale at regional flow system, local  or intermediate ones. The characteristic of the soil/rock material defines the conductivity, landscape position defines  the potential, and the climate controls the water input. This is applied widely until 1960s. Therefore, the groundwater discharge can be extended outside the basin hinge line (the upward/downward line), consequently the baseflow should not be simply described as the average recharge. 

Based on the predominate regional groundwater flow, three stream-aquifer systems are defined. 1) underflow-component dominated, which the ground water flows in the same direction of the streamflow. 2) baseflow-component dominated, which the groundwater is controlled by whether the stream is effulent or influent, the grounwater will be replinished or driven into the stream with a perpendicular direction. 3) Mixed

 

Mechanism of GW-SW interactions

Basic concepts

There are three ways for water entering the surface water body: 1. event flow/direct flow/storm flow/quick flow – individual water input events. 2. base flow – persistent, slowly varying sources and maintains stream flow between water-input events. 3. subsurface storm flow / interflow / return flow – water in the soil profile seepage into river. sometimes this is due to unsaturated and saturate flow that …..???!!!

 

Another four mechanisms that accounts for fast subsurface contributions to the storm hydrograph: 1) translatory flow - soil drainage to Field capacity, 2) macropore flow – rapid subsurface responses to storm inputs results from fast flow through larger noncapillary soil pores, 3) groundwater ridging – sudden increase of the hydraulic head after storms, 4) return flow – saturation excess surface-runoff production of the previous event when the water table and capillary fringe are close to the soil surface.

 

Large-scale interactions

Controlling factors of the large-scale interactions are, 1) hydraulic condictivities within channel and sediments, 2) stream stage to adjacent groundwater level, 3) geometry and position of channels. Directions of water flow are influent or effluent condition. Rainfall amount also controls the directions of water flow.  

groundwater exfiltration?

 

Discharge patterns could be perennial, intermittent, or ephemeral in time scale depend on the baseflow. Recharge of the flow can be parallel-flow channels, however flow-through channels pass through the river perpendicularly due to the elevation difference between banks. Thus it become flow-through reaches.   

 

Quantitative analysis

Key theoretical and field studies

 

Rest topics are out of my concerns for now…. 

Ecological significance of GW-SW interactions

Human impacts and water-resource depletion and sustainability

Human impacts

Water resources depletion and  sustainability

Conclusions and needed research

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Wiki

The River Continuum Concept (RCC) is a model for classifying and describing flowing water, in addition to the classification of individual sections of waters after the occurrence of indicator organisms[1]. The theory is based on the concept of dynamic equilibrium in which streamforms balance between physical parameters, such as width, depth, velocity, and sediment load, also taking into account biological factors[2]. It offers the introduction to map out pure living communities, but also an explanation for their sequence in individual sections of water. This allows the structure of the riverto be more predictable as to the biological properties of the water. The concept was first developed in 1980 by Robin L. Vannote, with fellow researchers at the Stroud Water Research Center [3].

 

Me,

River provides a continuum structure for organism. Every transition part between the headwater, midstream, lowerstream exist synchronized switch between types of resources retrieval organisms. Living consumers could be scrappers, collectors, and shredders; on the other hand, producers such as trees, periphyton, and phytoplankton play parts in this dynamics. Factors controlling this transition is derived from the continuum of structures like the size of particle organic matter

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This semester I am taking this discussion course. As "always", I am the dumbest person in discussing. I really like the material, the instructor, and the class; but the discussion is really overwhelming to me. Oh, I hate this..

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裸子植物的八個亞門
There are 8 subdivisions (亞門) within the division of Gymnospermae (裸子植物門). 

1 CYCADACEAE 蘇鐵科 2
2 TAXACEAE   紅豆杉科 3
3 AMENTOTAXACEAE 穗花杉科 4
4 CEPHALOTAXACEAE 三尖杉科
5
5 PODOCARPACEAE ____ 6
6 PINACEAE   __ 8
7 TAXODIACEAE __ 12
8 CUPRESSACEAE __ 14

Cycadaceae - tufted, pinnately compound leaves; The ovules and seeds (2-8) are born naked on the petioles of reduced leaves that are loosely clustered at the stem apex of female plants. Male plants produce male or microsporangiate cones that bear many scales. (excerpted from Hawaii.edu ) (microsporophyll ~ stamen; macrosporophyll ~ carpel)

1. CYCADACEAE 蘇鐵科 - 幹粗圓,直立。葉羽狀,螺旋排列於莖頂,葉柄基部宿存;小葉線形,近葉柄基部者退化成刺狀;鱗片葉小,前端長刺狀,密被褐毛。雌雄異株;雄球花長圓錐柱形,頂生;大孢子葉於莖頂螺旋狀排列成半球形,前方扁平呈闊卵形,邊緣羽狀分裂,小裂片成刺狀,尖銳,後方柄狀,柄之前方兩側共有胚珠3-5粒。

 

Taxaceae - Evergreen trees or shrubs, usually neither resinous nor aromatic (sharp- or foul-odored inTorreya), dioecious or monoecious. Bark scaly or fissured. Seeds 1 per "cone," erect, not winged, hard seed coat partially or wholly surrounded by a juicy, fleshy or leathery aril; cotyledons 2. Wood without resin ducts (Silba 1986Hils 1993). (the Gymnosperm Database)

2. TAXACEAE 紅豆杉科 - 喬木。葉線形,扁平,螺旋排列於小枝上,扭成不規則之2列,下表面氣孔帶淡黃綠色。雌雄異株;雄球花單一,腋生[size="7"],小孢子葉 6-14片[/SIZE],每片有 3-6個花粉囊;雌球花 1,腋生,胚珠 1,頂生於花軸上,被圍於杯形珠托內。種子堅果狀,包於紅色肉質假種皮內。

 

 

3. AMENTOTAXACEAE 穗花杉科 - 常綠小喬木。葉對生,線狀橢圓形或披針形,下表面中脈兩側各有1白色氣孔帶。雌雄異株;雄球花數個排成穗狀,數個穗狀花序簇生於枝頂,小孢子葉盾狀,有4-5個花葯。雌球花單生,有一彎曲之柄;胚珠單生於球花頂之中央,下方有6-10對苞片。種子核果狀,長橢圓形,由紅色假種皮包圍。

 


Cephalotaxaceae - These are much branched, small trees and shrubs. The leaves areevergreen, spirally arranged, often twisted at the base to appear 2-ranked. As the seed matures, the ovuliferous scale develops into a fleshy aril fully enclosing the seed. The mature aril is thin, green, purple or red, soft and resinous. 

Family Taxaceae Cephalotaxaceae
Cone aril partly encloses seed fully encloses seed
Cone maturation 6-8 months 18-20 months
Mature seed length 5-8 mm * 12-40 mm
(wiki)

4. CEPHALOTAXACEAE 三尖杉科 - 常綠喬木或灌木。葉線狀披針形,對生或近對生,下表面中脈兩側各有1白色氣孔帶。 雌雄異株或同株;雄球花6-11個聚生成頭狀,腋生;雌球花成頭狀,大孢子葉對生,頂端之數片各腋生2胚珠。種子1,由肉質假種皮包圍。

 

Podocarpaceae - Evergreen shrubs or trees, usually with straight trunk and more or less horizontal branches. Leaves usually spirally arranged, sometimes opposite, scale-like, needle-like, or more apart, flat and leaf-like, linear to lanceolate. Monoecious or dioecious. Pollen cones usually catkin-like; stamens numerous, close together, imbricate, each with 2 sporangia; pollen grains usually winged. All investigated Podocarpaeceae have vesicular-arbuscular mycorrhizas (Newman and Reddell 1987, Brundrett 2008 and citations therein)  (the Gymnosperm Database). (note: (AM fungi grows inside cortical cells of the root; it captures phosphorous and micronutrient from the soil - from wiki) 

5. PODOCARPACEAE 羅漢松科 - 小灌木或喬木。葉互生或對生。雌雄同株或異株;雄球花單或簇生葉腋,圓柱形,小孢子葉下部有 2花粉囊;雌球花單一,有柄,腋生;胚珠1,由珠套包圍,下方具1珠托。種子球形,外有肉質假種皮,下方有肉質或非肉質之種托。

 


6. PINACEAE 松科

 喬木;葉針或線形,單或簇生。雌雄同株;雄球花有許多螺旋著生之小孢子葉,每一小孢子葉有2花粉囊;雌球花有許多螺旋著生之大孢子葉;胚珠2,生於大孢子葉上表面近基部;苞鱗於大孢子葉下方。種子成熟時,大孢子葉增大且木質化;種子2,於種鱗之腋處,常有翅。

 台灣有6屬。


Useful link,
UCMP

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暑假, 雖然沒有上課, 但是每天的事情還是不斷, 我的步伐明顯緩和了許多, 但卻多了很多不確定; 不確定遠距離感情, 不確定研究的發展時程是否能達成期待,.... 兩週前, 看彼方的大哥跟阿廣都顯露出更多的疲憊, 聊賴, 還有慌忙; 我於是確定自己要出走BR城市。但說起來就是大方的有點不好意思: 作為一個正夾在油污事件與綠色能源發展之間的人類, 作什麼都不對。想不通, 我也只好暴走了。這是趟汽車之旅, 沒錯。


 


我飛往Wisconsin的老哥家, 氣溫27度, 十分宜人, 這趟旅程我都只有在晚間穿上pile, 大部份的時間都是曬太陽, 辨識植物, 跟健行。

行程: 
Day1. New Orleans Int'l Airport. Missed my original flight and waited for 6 hours to switch to another longer flight. I spent total 27 hrs from my BR apt to my brother's house in Madison........  Next time I have to recheck if I check in before I drive! It is wasting time in the airport! By the way, the carry-on luggage is free (22*14*9 inches for Delta)... I shouldn't have carried such a heavy bag. As for the rescheduling, call the counter is always faster than waiting in line. If you cannot make it to stand in line, I bet you would like to make a call first. To reschedule, they allow you to do that within 3 hours and charge you only 50 dollars. 
 

Day2. Madison --> Fishcreek (4hrs drive): Peninsula State Park
Hiking on the Eagle Cave, Camping at the Tennison Bay (#212 near the bay; the site was too humid.)
The trail is very awesome! But you wouldn't want to hike it during sunset... because the sunlight would be already on the back side of the cliff. This trail is famous for the cliff. They are limestones. White Cedar and Hemlock forest live upon the rock. We both think it is just like the "天空の城ラピュタ". It also looks so much like the 空島 in One piece. 

Day3. Penin SP.: Kayak & Bicycling! (Kayaking to the Eagle Cave, spending 1.5hrs; Cycling on the Sunset trail, many tourists)
Renting a Kayak and bikes are actually affordable. My brother really enjoyed the sceneries! Good for him!

半島公園

 

 

 


Day 4. Madison -->Boston city (arrived at 7:30pm) ---> Concord, NH (1.5hrs drive)

去白山的旅程比較樸實, 我們幾乎都在車上觀看景物, 因為我待留時間太短, Frog不想紮營, 早上他賴床, 所以根本沒空去走個trail. 最後是開車到白山頂上逗留兩個小時, 看看背著重裝歐洲人緩步前行的樣子, 還有跟印度人搶著跟Peak牌子拍照, 然後追著鐵路小火車, 完成這整趟白山假攻頂之旅。

回程的路上我們逗留了兩個臨時景點, 從恰克湖看著落日夕陽下的華盛頓山, 很愜意; 本來以為趕不上在波士頓的煙火秀了, 沒想到竟然在US-25的路上行經幾個港口, 那幾個小鎮還真有錢呢, 花火不斷, 我跟阿廣就在岸邊湊湊熱鬧囉。一點都不擠呢。 

Day 5. White Mt. area 
                            Wondering around the view and finally got up on the White Mt. Auto Road, 
                            Overlooking on Mt. Washington (Peaked at 1917m)
                            Passing by Chocorua Lake and found a small Droseraceae plant!
                            Stopped at Center Harbor, participating the Fireworks! Great!
Day 6. Flight back home. Exhausted!        

 

白山森林

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Today, I am listening to NPR radio about the oil spill event. 
Talk the Nation is a good program,

It is a talk between Rebecca Roberts and Lisa Margonelli, executive director of the New America Foundation's energy initiative, "Lisa Margonelli is director of the New America Foundation's energy initiative and author of "Oil on the Brain: Petroleum's Long, Strange Trip to your Tank.""

Topic: Op-Ed: Oil Drilling Unsafe In Every Backyard

(Related opinion, "A spill of our own")

(2010.05.03)

ROBERTS: We have email from Richard(ph) in Ann Arbor, who says, in January, Cuba announced they would drill in the Strait of Florida. Mexico presumably drills of its ghost coast, which is - gulf coast - which is at least as long as ours. Does anyone rationally believe that a moratorium on the part of the U.S. will deter any other players in the Gulf from drilling?

Ms. MARGONELLI: No.

(Soundbite of laughter)

ROBERTS: That's a succinct answer.

 

-Sum-up- Major questions: 

1. The first moratorium was after the 1969 blowout and giant spill in Santa Barbara, which also was the foundation of Earth Day. 
    I mean, it's fine if we want to have some sort of moratorium, but the bigger underlying problem is that our gasoline consumption continues to rise. 

2. what we need is a comprehensive way - some sort of comprehensive legislation addressing a plan to decrease our oil consumption.
==> a. One is to obviously raise the CAFE standards, another one is all the sorts of things that we did in the '70s with, you know, changing the speed limit to 55 and retiming the stops - the traffic lights. And there are lots of things that we can do to change traffic flow, but we can also do things like natural gas trucking and some alternative fuels.
b. A company like Wal-Mart, for example, has 1.4 million employees. If they ran van pools to get them to work, it would remove a tremendous number of cars from the road and really ease the burden on the workers, of maintaining, oftentimes old cars, and paying for the gasoline when prices are high.

3. oil spills are predictable. It's true. Oils - no - every oil spill is preventable. But oil spills are, essentially, inevitable. And the industry itself measures the rate of spill per ton-mile shipped. 

4. I think push for a conversation that leads to specific policy initiatives and a real commitment to reducing our dependence on oil, 
..... I think this is sort of one of these catalytic moments when we could really address this problem. 

5.  I think that one group that has a really hard time with high gas prices is working families, what we would call maybe the middle class or lower middle class......

6. I think that we do need to reform drilling policy.  
One of the things that sticks out is, you know, after the Exxon Valdez, we reformed oil shipping with an act called the Oil Pollution Act of 1990 (OPA 90 Act)- that really dramatically reduced spills.

7. But the Minerals Management Service is a notoriously troubled agency. 
...... partly through some complexes exchanges that the Minerals Management Service is okay with; but partly because we simply don't charge them enough. And we might be missing out on 100 to $400 billion worth of extra payments, which is really appalling.

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1. Largest Oil Spill occurred in the Gulf of Mexico which was nearly 50 km from the coastline.  

2. Oil Rig Sinks, as Does Senate Climate Bill

3. What's Behind the Honeybee Decline? Perhaps Not What You've Heard

4. Germany's first offshore wind farm begins turning

5. Environmental lawsuit claims Massey pollutes water 

 6. Can Global Warming Give You Kidney Stones? How Will Insurance Companies Deal With Rising Temperatures?

7.【APGN在台灣】國內環境急惡化 各國盼以國際力量影響政府

  【APGN在台灣】吐瓦魯總理:滅國迫在眉睫 氣候談判緩不濟急

   【APGN在台灣】開放空間會議 以多元、開放自由的原則產出決議

8. 物種消失未減緩 2010全球保育任務失敗!

9. 東非的綠色農業大躍進

10. 印度新德里發現放射性廢物 1人死亡6人住院



‎Ref: e-info, ENS, & Google

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