Determination of species-area relationships and minimum sampling area for the shrub communities in the arid valley in the upper reach of the Minjiang River, China

2007 ◽  
Vol 27 (5) ◽  
pp. 1818-1825 ◽  
Author(s):  
Chen Hong ◽  
Li Yanqiong ◽  
Zheng Shaowei ◽  
Wang Ling ◽  
He Fei ◽  
...  
PeerJ ◽  
2020 ◽  
Vol 8 ◽  
pp. e8957 ◽  
Author(s):  
Roberto C. Hernández-Landa ◽  
Erick Barrera-Falcon ◽  
Rodolfo Rioja-Nieto

The characterisation of changes in coral communities depends heavily on systematic monitoring programs and the collection of necessary metrics to assess reef health. Coral cover is the most used metric to determine reef health. The current organizational shift in coral requires the evaluation of complementary metrics, such as colony size and frequency distributions, which help to infer the responses of the coral populations to local stress or larger scale environmental changes. In this study, underwater digital photogrammetry techniques were used to assess the live cover of all coral colonies ≥3 cm2 and determine the size-frequency distribution of the dominant species in the shallow reefs of the Cozumel Reefs National Park (CRNP). In addition, the minimum sampling area (m2) needed to obtain a representative sample of the local species pool was estimated. Areas between 550 and 825 m2 per reef were photographed to generate high-resolution digital ortho-mosaics. The live area of the colonies was digitised to generate community matrices of species and abundance. EstimateS software was used to generate accumulation curves and diversity (Shannon H′) at increasing area intervals. Chi-Square tests (χ2, p = 0.05) were used to compare the observed vs estimated species richness. Spearman’s coefficients (rs), were calculated to correlate the increase in sampling area (m2) vs H′, and the Clench’s function was used to validate the observed richness (R2 = 1 and R > 90%). SIMPER analysis was performed to identify dominant species. Comparisons in terms of abundance, coral cover and size-frequencies were performed with Kruskal-Wallis (H test, p = 0.05), and paired Mann-Whitney (U test, p = 0.05). In order to obtain 90% of the species richness, a minimum sampling area of 374 m2is needed. This sampling area could be used in shallow Caribbean reefs with similar characteristics. Twelve (mainly non-massive) species: Agaricia agaricites, A humilis, A. tenuifolia, Eusmilia fastigiata, Meandrina meandrites, Montastrea cavernosa, Orbicella annularis, Porites astreoides, P. porites, Pseudodiploria strigosa, Siderastrea radians andS. siderea, were dominant in terms of abundance and coral cover. A significant increase (p < 0.05) in the number of colonies and live coral (m2) was observed from north to south of the study area. Furthermore, a wide intraspecific variation of size-frequency, even between adjacent reefs, was also observed. The size-frequency distributions presented positive skewness and negative kurtosis, which are related to stable populations, with a greater number of young colonies and a constant input of recruits. Considering the increase in disturbances in the Caribbean and the appearance of a new coral disease, digital photogrammetry techniques allow coral community characteristics to be assessed at high spatial resolutions and over large scales, which would be complementary to conventional monitoring programs.


2021 ◽  
Vol 913 (1) ◽  
pp. 012095
Author(s):  
K Senjarini ◽  
R Setiawan ◽  
S Wathon ◽  
R Oktarianti

Abstract Malaria’s cases have been reported to occur annually in Wongsorejo district of Banyuwangi, East Java since 2002. However, there is a significant decrease of malaria cases during these last years, which might be related to the malaria vector species shifting composition. The objective of this research was to observe some important bionomic characteristics of malaria vector Anopheles in this area from 2015 until 2020 which include species identification, blood feeding behaviour and biting preference of vector. The data collection i.e. determination of Anopheles diversity and behaviour was conducted monthly for 3-6 months annually from 2015 – 2018. In 2019-2020 we sampled irregularly to see the trend. The results showed that there were species shifting of Anopheles vectors in this area. The proportion of Anopheles (An.) sundaicus and An. subpictus, which were previously reported until 2015 as the main Anopheles species in this area, significantly decreased in 2016 - 2018. An. indefinitus & An. vagus was becoming the majority of Anopheles species. During 2019-2020, An. vagus became the main species identified in the sampling area. The predominant species of An. vagus and An. indefinitus has exophagic and zoophilic preference behaviour. Furthermore, An. indefinitus has not previously been identified as a vector for malaria, compared to An. sundaius, and An. subpictus which are well known as an important primary malaria vector on Java Island, Indonesia.


1984 ◽  
Vol 35 (5) ◽  
pp. 645 ◽  
Author(s):  
F Forcella

A species-area curve was constructed for buried viable weed seeds in a 5-year-old subterranean clover-annual ryegrass pasture in south-eastern Australia. A soil surface area of about 200 cm2 (to a depth of 10 cm) was required to obtain a representative individual sample (i.e. a replicate) of the number of taxa in the soil seed bank, whereas a combined area of about 1000 cm2 was required for adequacy within any treatment. The total number of buried viable seeds of all species combined was distributed spatially in a more-or-less uniform manner. This suggests that a sample whose size is sufficient for determination of species diversity of buried seeds is equally adequate for measuring buried seed density.


Fractals ◽  
1999 ◽  
Vol 07 (04) ◽  
pp. 353-357 ◽  
Author(s):  
KAZUHITO YAMASAKI ◽  
SATOSHI CHIBA ◽  
HIROYUKI NAGAHAMA

We introduce a new immigration model which merges two aspects of island length. One aspect is determination of colonizer's chance of reaching recipient island, and the other is constraint on the statistical self-affinity (anisotropy) of island shapes. This immigration model derives the famous power law on species-area (SA) relation, which shows that the number of species on the anisotropic island is constrained by not only the size of the island area but also the shape of the island. From this viewpoint, we analyze an SA curve of the land snail fauna in Ryukyu arc, Japan. Moreover, we show that species of the most previous studies have immigrated along the island chain due to the stepping-stone dispersal.


2018 ◽  
Vol 6 (1) ◽  
pp. 8
Author(s):  
Prama Widayat

The research was conducted to observe the implementation of risk management in analyzing the contractor before issuing Surety Bond guarantee by the insurance and continue as the basis for the issuance of Bank Guarantee (KGB) by private banks and BUMN, because there are still contractors who do not perform their obligation to finish the work causing the claim bank guarantee product. The study was conducted by direct interviews to underwriting insurance issuing Bank Guarantee Cons (KGB) products. The study population amounted to about 67 insurance companies registered in Riau province. But not all of them publish KGB is only 5 general insurance companies, the determination of the number of samples is done by using the sampling area.


2021 ◽  
Author(s):  
Tim Kerlin ◽  
Mark Musall ◽  
Peter Oberle ◽  
Franz Nestmann

&lt;p&gt;Within the joint project Integrated Water Governance Support System (iWaGSS) funded by the German Federal Ministry for Education and Research (BMBF, reference numer: 02WGR1424C) the Institute of Water and River Basin Management (IWG) of the Karlsruhe Institute of Technology (KIT) developed a benthic flume. The benthic flume HIPPO (Hydro-morphological Investigation of riverbed Particle Performance On-site) is an adjustable in situ device to reliably determine the start of erosion of fine sediments.&lt;/p&gt;&lt;p&gt;In advance 3D-CFD simulations have been carried out to optimize the components and the setup of the measurement system. The final product is primarily a benthic flume, which has a downwardly opened sampling area at the bottom and is placed on the river or reservoir bed. This underwater flow channel can be adapted to the local conditions with further components and is connected via a tube system to a measurement boat or raft. On the boat a pump creates a steady flow velocity in the system. The velocity in the benthic flume is gradually increased at fixed time intervals and is monitored using a built-in flow velocity meter (Acoustic Doppler Velocimeter). In addition the entire erosion process is recorded visually with video cameras. Also the turbidity of the water flowing through the system is continuously measured by a turbidity probe installed behind the pump. The amount of flow induced by the pump is controlled by a valve close to the end of the system. With the pump currently installed flow velocities of up to v = 0.8 m/s at the sampling area can be achieved, which is sufficient for the determination of the critical flow rate for erosion of most types of clay, silty and fine sandy sediments. During the process of erosion also the remobilization of fluid mud can be monitored. The critical flow velocity for the start of sediment transport is determined on the basis of the turbidity of the pumped water and data from the flow velocity probe and is verified using the camera system.&lt;/p&gt;&lt;p&gt;In addition to the critical threshold flow velocities, the critical bed shear stress is often required as input or evaluation variables for morhpodynamic numerical models. The conversion can be made, for example, using the quadratic velocity approach originally used in pipe hydraulics. The determination of the required resistance coefficient &amp;#955; is based on the Moody Chart. However, it should be considered that this procedure entails some uncertainties with regard to the measurement system presented here. Still for cohesive sediments, the natural values measured in this way represent a significant added value compared to common estimates based on only partially known bed parameters, since factors such as vegetative cover, consolidation or even a developed biofilm can influence the timing of erosion. Especially against this background, possible effects of the change of hydraulics by the measuring system (geometry, velocity profile) seem to be small compared to the uncertainties of contemporary morphodynamic analyses.&lt;/p&gt;


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