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What a paediatrician should know about congenital clubfoot Daniela Dibello1, Valentina Di Carlo1, Giulia Colin2, Egidio Barbi1,2 and Anna M. C. Galimberti2*

Abstract

Clubfoot is the most frequent congenital malformation of the foot, affecting more than 1–2 subjects per 1.000 newborns. Without appropriate treatment, a child with congenital clubfoot will never be able to walk physiologically with a dramatic impact on the quality of life. In the last decades, different corrective solutions have been proposed, and there is rising scientific evidence that the Ponseti non-invasive method is safe and effective in the treatment of the clubfoot. So, what should a general paediatrician know about this condition and what should he concretely do in the suspect of a congenital clubfoot?

Keywords: Clubfoot, Talipes, Equinovarus, Management, Pediatric

Background The talipes equinovarus congenital foot, also known as congenital clubfoot, is the most common congeni- tal malformation of the foot. One or two, per 1000 newborns are affected [1], with a male to female ra- tio of 1 to 2. This condition is particularly frequent in Developing Countries (80% of overall cases). In 50% of cases, it affects both feet [2]. Without ad- equate treatment children with congenital clubfoot will not walk physiologically and will not be able to live a normal life. Paediatricians have a critical role in the early detection of this condition, starting from the first evaluations of the newborn. The prompt re- ferral to the specialist is crucial for these children to obtain a plantigrade and functional foot. This article aims to provide the general paediatrician with essen- tial knowledges for proper clubfoot management. The scientific literature supports the efficacy of Pon- seti method for this pathology, and we tried to sim- plify and explain the therapeutic process and the general management.

What is clubfoot? Congenital clubfoot is a malformation characterized by a torsion of the longitudinal axis of the foot, secondary to a malalignment of the calcaneo-talar-navicular complex. The foot’s sole is rotated medially and this leads the child to walk on the foot sides (Fig. 1). We can detect four different anomalies; CAVE is a mnemonic tip to re- member them all (Fig. 2):

1. Midfoot cavus deformity (the sole of the foot “looks” upwards).

2. Metatarsus adductus (the fingers point inside with concavity of the medial foot margin).

3. Hindfoot varus deformity (medial deviation of the longitudinal axis of the calcaneus).

4. Hindfoot equinus deformity (extreme plantar flexion).

There are two main types of congenital clubfoot: idio- pathic (80% of cases) and secondary clubfoot (20% of cases). The idiopathic congenital clubfoot is a multifac- torial condition that includes environmental, vascular, positional, and genetic factors. Clubfoot has a tendency to segregate in families: the risk of developing congenital clubfoot is 25% when a first-degree relative is affected.

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* Correspondence: annamachigalimberti@gmail.com 2University of Trieste, Piazzale Europa 1, Trieste, Italy Full list of author information is available at the end of the article

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Several studies and observations suggest the exist- ence of different genes and inheritance patterns in- volved [3]. On the other hand, up to 20% of cases of congenital clubfoot is associated to other anomalies (e.g., myelomeningocele) and could be secondary to a specific genetic condition such as Moebius syn- drome, neurofibromatosis and multiple congenital arthrogryposes [4]. The congenital clubfoot could also show more complex anatomic features that typ- ically present a shorter and more rigid foot, in which there is a marked curvature of the midfoot (metatar- sal equinism) with deep skin folds. In these cases we talk about an “atypical clubfoot” [5]. Clinical features of clubfoot may already emerge in prenatal diagnos- tics, but its ultrasonographic diagnosis appears more likely between the 18th and the 24th week of preg- nancy [6].

How to perform a focused examination? The foot needs to be evaluated in their complexity: general morphology, presence of skin folds, muscu- lar and tendon malleability and flexibility of the

Fig. 1 Frontal and posterior view of congenital idiopathic clubfoot

Fig. 2 Severe clubfoot. legend: severe clubfoot (Pirani 6, Manes-Costa 3)

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deformation. Flexibility is the most relevant element that influences the prognosis: the more malleable and easy to move the foot, the better the prognosis. There are several classification systems of the club- foot, for example Manes-Costa’s classification, Pira- ni’s score (Fig. 3) or Dimeglio classification. These scores are valid prognostic tools and can be used in the follow-up process. A high score at presentation may indicate that a longer and more complex treat- ment will be required. Whenever a congenital club- foot is detected, a complete examination is mandatory to rule out other neuro-musculoskeletal problems, such as signs of occult spinal dysraphism, developmental dysplasia of the hip (DDH) or con- genital torticollis. It is essential to differentiate clubfoot from two

other disorders: postural equino-varus foot and metatarsus adductus. The postural equino-varus is a functional malposition of the foot caused by the de- formed position that the fetus used to hold in the maternal womb. In this case, there may be some

degrees of forefoot adduction, but it will be flexible at the manipulation, and there will be no Achilles tendon contracture. Generally, the postural equino- varus resolves spontaneously; nevertheless, it is good practice to monitor the progression (in premature newborn, a clubfoot can sometimes hide behind a postural equino-varus) [7]. The adductus metatarsus is another common deformity characterized by an adducted forefoot with a curvature of the lateral edge of the foot, but without the other features of clubfoot. Also, this disorder is secondary to the intrauterine postural modeling of the feet and gener- ally resolves spontaneously (casting may be necessary if the deformity is rigid).

Which therapy? Over the decades the surgical treatment of congeni- tal clubfoot has mostly been abandoned, as it was associated with complications, with the final result of a foot that would hardly reached full functional- ity, due to retractions and scars, secondary to the

Fig. 3 Pirani clubfoot- score. legend: this is a 6-item scale, in which every point has a 0 to 1 score (0 if normal, 0.5 if moderate-mild deformity is present, 1 with a severe malformation); the higher the score is, the worst is the deformity

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surgery itself. Although some complex and atypical clubfeet still need surgical treatments at first [7], the available evidence has definitively confirmed the effectiveness of the Ponseti non-invasive method [1, 8, 9]. It consists of gentle manipulations of the foot followed by the application of plaster casts, which are kept in place for 5-7 days, during which muscles and ligaments adapt to the new position. At the end of the 5-7 days period, the cast is removed, the foot (which would become softer and more prone to be moulded) is revaluated and progressively manipu- lated to maintain, through the application of a new cast, a new position [2, 8]. The procedure is re- peated until normal foot alignment is achieved (on average, about five to six plaster casts are required). Percutaneous Achille’s tenotomy (Fig. 4) could be required if equinus deformity persists at the end of the casting phase. The procedure takes about 5 min and consists of a millimetric posterior skin incision through which the tendon section is achieved. After the tenotomy, plaster is applied to allow the tendon to heal in elongation for about 20 days. In order to maintain the correct position of the foot,it is neces- sary to wear, an orthopedic brace until 5 years of age. The brace must be worn for 23 h a day for the first 3 months. Over time, the child may gradually decrease the use of the brace during the day:: after the first months, it is necessary to wear the cast for at least 18–19 h with a gradual reduction in the use of 1 h per month up to a maximum of 12 h without the brace. When the patient begins to walk inde- pendently, the brace is usually only held overnight until the age of five.. Compliance with the splinting

programme is crucial to prevent recurrences [10], and the general paediatrician has a critical role in supporting the family during the brace-phase. To conclude, the treatment of an “atypical clubfoot” is

more challenging and difficult and often requires a higher number of plaster casts.

What management should a paediatrician provide? Radiological diagnostic evaluations, such as foot X- rays or ultrasounds, are usually not necessary in addition to the clinical assessment. In the case of very complex clubfoot, it could be reasonable to evaluate the possibility of an underlying process or other associated malformation. A co-existent hip dysplasia, myogenic torticollis, or other orthopedic conditions should always be ruled out. The paedia- trician also has to evaluate the child to exclude a systemic condition (such as a neuromuscular disease or a syndromic illness – see Table 1). Paediatricians are also in charge of preparing the family for the therapeutic process. Reassurance and providing a direct link to an experienced centre are the first steps. Operational timeliness is essential in terms of outcomes so the newborn needs to be referred to the specialist as soon as possible, e.g., in the very first days of life. The relapses of the clubfoot are not uncommon (about 5–10%), either with conser- vative and surgical methods. Consequently, paedia- tricians should play a relevant role in supporting the family and monitoring compliance with the con- stant use of the orthopedic brace, which represents the main factor in preventing the recurrence of malformation.

Four golden rules for an adequate approach

1. The earlier, the better: if you detect a clubfoot contact a local orthopedic surgeon who can take care of the referral to a clubfoot center, preferably within 48 h but not more than 1 week after the delivery [7];

2. Motivate the parents: to improve the compliance with the use of the brace to minimize the recurrences [7];

3. In case of a severe clubfoot: inform the parents of the increased risk recurrences;

4. Clubfoot is diagnosed through clinical evaluation, and usually, a radiological evaluation is not necessary. The orthopedic surgeon can choose to perform a radiological evaluation in selected cases (e.g., in front of a weak response to treatment or severe relapses) [7].

Fig. 4 Percutaneous tenotomy of the Achille’s tendon

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Conclusion Clubfoot is a highly invalidating condition all over the world; the absence of an adequate treatment will lead to dramatic consequences on the quality of life of the patients, with a high social burden. The rapid recog- nition of deformity and immediate reference to the orthopedic specialist are the key elements for effective treatments.

Acknowledgements The authors thank Martina Bradaschia for the English revision of the manuscript.

Authors’ contributions All authors contributed and approved the final manuscript.

Funding None.

Availability of data and materials Not applicable.

Ethics approval and consent to participate Not applicable.

Consent for publication Obtained.

Competing interests The authors declare that they have no competing interests.

Author details 1Institute for Maternal and Child Health IRCCS Burlo Garofolo, Via dell’Istria 65/1, Trieste, Italy. 2University of Trieste, Piazzale Europa 1, Trieste, Italy.

Received: 27 March 2020 Accepted: 25 May 2020

References 1. Balasankar G, Luximon A. Ponseti method in the management of clubfoot

under 2 years of age: A systematic review. PLoS One. 2017;12(6):e0178299. 2. Balasankar G, Luximon A. Current conservative management and

classification of club foot: A review. J Pediatr Rehabil Med. 2016;9(4):257–64. 3. Basit S, Khoshhal KI. Genetics of clubfoot; recent progress and future

perspectives. Eur J Med Genet. 2017;61(2):107–13. 4. Pavone V, et al. The etiology of idiopathic congenital talipes equinovarus: a

systematic review. J Ortho Surg Res. 2018;13(1):206.

Table 1 from B. Sadler, C. A. Gurnett, and M. B. Dobbs “The genetics of isolated and syndromic clubfoot”, Journal of Children Orthopaedics Jun 2019

Condition/syndrome name Known genes

Autosomal Dominant Larsen Syndrome, Recessive spondylocarpotarsal syndrome FLNB

Barth Syndrome TAZ

Bruck Syndrome PLOD2, FKBP10

Carey-Fineman-Ziter Syndrome MYMK

Catel-Manzke Syndrome TGDS

Charcot-Marie-Tooth Disease Type 4D NDRG1

Diastrophic dysplasia SLC26A2

Ehlers-Danlos Syndrome, Musculocontractural type 1 CHST14

Ehlers-Danlos Syndrome, Musculocontractural type 2 DSE

Ehlers-Danlos Syndrome, vascular type COL3A1

Epileptic Encephalopathy AARS

Joubert Syndrome ATXN10, TCTN2

Loeys-Dietz Syndrome TGFBR1, TGFBR2, SMAD3, TGFB2, TGFB3

Marfan Syndrome FBN1, TGFBR, TGFBR1, TGFBR2, SMAD3, TGFB2, SKI

Moebius Syndrome PLXND1, REV3L

Multiple Epiphyseal Dysplasia COL9A1, COL9A2, COL9A3, COMP, MATN3, SLC26A2

Multiple Synostosis Syndrome GDF5

Peroxisome biogenesis disorder 7A PEX26

Recessive axonal Charcot-Marie-Tooth Disease LMNA, GDAP1

Recessive Larsen Syndrome, Humero-Spinal Dysostosis, Spondyloepiphyseal dysplasia CHST3

Richieri-Costa – Pereira Syndrome EIF4A3

Santos Syndrome WNT7A

Saul-Wilson Syndrome COG4

Schpritzen-Goldberg Syndrome SKI

TARP Syndrome RBM20

Van Maldergem Syndrome 2 DCHS1, FAT4

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5. Van HJP B. Challenging clubfeet: the arthrogrypotic clubfoot and the complex clubfoot. J Child Orthop. 2019;13(3):271–81.

6. Faldini C, et al. Prenatal Diagnosis of Clubfoot: A Review of Current Available Methodology. Folia Med. 2017;59(3):247–53.

7. Besselaar AT, Sakkers R. JB et al. guideline on the diagnosis and treatment of primary idiopathic clubfoot. Acta Orthopaedica. 2017;88(3):305–9.

8. Chu A. Treatment of Idiopathic Clubfoot in the Ponseti Era and Beyond. Foot Ankle Clin. 2015;20(4):555–62.

9. Morcuende JA, Dolan LA, Dietz FR, Ponseti IV. Radical reduction in the rate of extensive corrective surgery for clubfoot using the Ponseti method. Pediatrics. 2004;113(2):37680.

10. Staheli L, Ponseti I, Morcuende JA, et al. Clubfoot: Ponseti management. 3th edition, Global HELP Ed, 2009.

Publisher’s Note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

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  • Abstract
  • Background
    • What is clubfoot?
    • How to perform a focused examination?
    • Which therapy?
    • What management should a paediatrician provide?
    • Four golden rules for an adequate approach
  • Conclusion
  • Acknowledgements
  • Authors’ contributions
  • Funding
  • Availability of data and materials
  • Ethics approval and consent to participate
  • Consent for publication
  • Competing interests
  • Author details
  • References
  • Publisher’s Note

Decreased abundance of crustose coralline algae due to ocean acidification

© 2008 Nature Publishing Group

LETTERS

Decreased abundance of crustose coralline algae due to ocean acidification

ILSA B. KUFFNER1*, ANDREAS J. ANDERSSON2,3*, PAUL L. JOKIEL4, KU‘ULEI S. RODGERS4

AND FRED T. MACKENZIE2 1US Geological Survey, Florida Integrated Science Center, St Petersburg, Florida 33701, USA 2University of Hawaii, Department of Oceanography, 1000 Pope Road, Honolulu, Hawaii 96822, USA 3Bermuda Institute of Ocean Sciences, 17 Biological Lane, St George’s, GE01, Bermuda 4Hawaii Institute of Marine Biology, PO Box 1346, Kaneohe, Hawaii 96744, USA *e-mail: ikuffner@usgs.gov; andreas.andersson@bios.edu

Published online: 23 December 2007; doi:10.1038/ngeo100

Owing to anthropogenic emissions, atmospheric concentrations of carbon dioxide could almost double between 2006 and 2100 according to business-as-usual carbon dioxide emission scenarios1. Because the ocean absorbs carbon dioxide from the atmosphere2–4, increasing atmospheric carbon dioxide concentrations will lead to increasing dissolved inorganic carbon and carbon dioxide in surface ocean waters, and hence acidification and lower carbonate saturation states2,5. As a consequence, it has been suggested that marine calcifying organisms, for example corals, coralline algae, molluscs and foraminifera, will have difficulties producing their skeletons and shells at current rates6,7, with potentially severe implications for marine ecosystems, including coral reefs6,8–11. Here we report a seven-week experiment exploring the effects of ocean acidification on crustose coralline algae, a cosmopolitan group of calcifying algae that is ecologically important in most shallow- water habitats12–14. Six outdoor mesocosms were continuously supplied with sea water from the adjacent reef and manipulated to simulate conditions of either ambient or elevated seawater carbon dioxide concentrations. The recruitment rate and growth of crustose coralline algae were severely inhibited in the elevated carbon dioxide mesocosms. Our findings suggest that ocean acidification due to human activities could cause significant change to benthic community structure in shallow-warm-water carbonate ecosystems.

Crustose coralline algae (CCA) are a major calcifying component of the marine benthos from tropical to polar oceans at all depths within the photic zone in almost every habitat type13–15. CCA carry out key ecological roles on coral reefs, such as acting as framework organisms, cementing carbonate fragments into massive reef structures16, providing chemical settlement cues for reef-building coral larvae17,18 and as major producers of carbonate sediments12. So far, the main focus of global climate change research on coral reefs has been the impact of rising temperatures on coral ‘bleaching’ and mortality, but lately the effects of ocean acidification have received increased attention7,8. Experimental work has demonstrated that corals calcify more slowly under conditions of elevated partial pressure of carbon dioxide (pCO2) and lower calcium carbonate saturation state

6,19, and studies have shown similar results for select species of calcifying macroalgae cultured in small incubation vessels20,21. The purpose of

our flow-through outdoor mesocosm experiment was to provide empirical quantification of changes to benthic communities that may result from the decrease in calcium carbonate saturation state predicted for tropical and subtropical oceans over the next centuries. Our approach was novel in that the experiment was conducted in an outdoor flow-through system, enabling organisms with pelagic larvae to settle in the mesocosms and develop communities as natural recruitment occurred over several months. The mesocosms were designed to experience natural diurnal cycles in solar radiation, temperature and seawater chemistry typically occurring on tropical reef flats. Although previous work examined the effects of calcium carbonate saturation state on calcification rates of corals and coral communities in realistic mesocosm studies9,10,19,22, none has examined how community structure may change under increasing degree of ocean acidification.

Our mesocosms showed marked diurnal cycles in seawater chemistry (Fig. 1) similar to those observed on other tropical reef flats (for example 1 0.6 pH units23). The encrusting algal community that recruited to acrylic cylinders placed in the treatment mesocosms was quite different from that found on cylinders from control mesocosms (Fig. 2). The recruitment rate and the percentage cover of CCA on cylinders in treatment mesocosms at the end of the 51 d period were significantly lower than those in controls (Fig. 2a–c, Table 1). Mean percentage cover by non-calcifying algae (a mixed assemblage of macroalgal germlings, diatoms and small filamentous algae) was statistically higher on cylinders from treatment compared with control mesocosms (Fig. 2d, Table 1). Under high pCO2 conditions, CCA recruitment rate and percentage cover decreased by 78% and 92%, respectively, whereas non-calcifying algae increased by 52% (Fig. 2) relative to controls. Decreased rates of space occupation by CCA imply inhibition of growth and/or calcification, indicating that at least one step in the calcification process is being directly affected; however, the cellular and molecular mechanisms of calcification in these organisms remain elusive6,24.

At tropical and subtropical seawater conditions, CCA and many important reef calcifiers such as echinoderms, other calcifying algae and benthic foraminifera deposit Mg calcite minerals that contain significant mol% MgCO3. CCA in the present study contained 13.6 ± 0.4 mol% as determined from X-ray diffraction (XRD) analysis (see the Supplementary Information), and there was no

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Feb-01 Feb-15 Mar-01 Date

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Figure 1 Seawater carbonate chemistry. Data observed at midday (a–d) and during a diurnal cycle (e–h) in control (circles) and treatment (squares) mesocosms. a,e, Partial pressure of CO2 (pCO2); black dots are surface seawater values reported by the CRIMP/CO2-NOAA PMEL buoy. b,f, Saturation state (Ω) with respect to 13.6 mol% Mg calcite. c,g, pHNBS. d,h, Total alkalinity (TA). Data are means ±1 s.d. (n = 3 mesocosms). Dashed lines are values projected for the year 2100 (IPCC, IS92a). See Supplementary Information for tabulated data.

significant difference between treatment and control samples. Our results contrast with those of refs 20 and 25, which reported that the Mg content of the calcifying alga Porolithon gardineri varied positively with seawater calcite saturation state, temperature and growth rate. The mechanisms controlling the concentration of Mg ions in the mineral structure of biogenic calcites are not well understood and probably exert different influences on different organisms26. Large variability in the Mg content among different taxa living in the same environment suggests that there is strong taxonomic control12. Geographically, there is a convincing correlation between Mg content within taxonomic groups and environmental parameters such as temperature and seawater carbonate saturation state. This correlation has been

attributed to growth rate, which is a function of temperature and carbonate saturation state26. Control of Mg content in marine calcifiers warrants further investigation, as the amount of Mg incorporated in the mineral matrix directly affects its solubility. Biogenic Mg calcite phases containing a significant mol% MgCO3 (>8–12 mol%) are more soluble than aragonite, the carbonate phase deposited by corals, and could initially be more susceptible to rising pCO2 and decreasing seawater calcium carbonate saturation state27,28. Nevertheless, the changes in seawater chemistry anticipated during the 21st century under the business- as-usual CO2 emission scenario are sufficiently large to affect significantly both aragonite and Mg calcite precipitation rates and the organisms depositing these minerals.

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C1 C2 C3 T1 T2 T3 C1 C2 C3 T1 T2 T3

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Figure 2 Encrusting algal communities on experimental cylinders. Recruitment rate (a) and percentage cover (b) of CCA on cylinder surfaces from control (white bars) and treatment (black bars) mesocosms. c, Photograph of example cylinders from a control (left) and a treatment (right) mesocosm. d, Percentage cover of non-calcifying algae on cylinder surfaces from control (white bars) and treatment (black bars) mesocosms. Data are means ±1 s.d. (n = 3 cylinders). C = control and T = treatment, and the number refers to the replicate mesocosm. See Supplementary Information for tabulated data.

Table 1 Mean seawater carbonate chemistry near midday (n = 11 sample days), rate of CCA recruitment and percentage cover by CCA and non-calcifying algae found on experimental cylinders in control and treatment mesocosms, and accompanying statistical tests.

Control Treatment One-way analysis of variance A priori contrast n = 3 (ANOVA) by mesocosm between treatment

Mean (± 1 s.d.) and control mesocosms

F P t P

pCO2 (µatm)∗ 400 (47) 765 (39) 49.2 <0.0001 8.35 <0.0001 Saturation state 2.74 (0.21) 1.55 (0.06) 53.8 <0.0001 8.10 <0.0001

(13.6 mol% Mg calcite)∗ pHNBS∗ 8.17 (0.04) 7.91 (0.02) 53.7 <0.0001 8.52 <0.0001 Total alkalinity (µmol kg−1) 2,156 (2.1) 2,016 (9.2) 45.7 <0.0001 4.29 = 0.0001 CCA (recruits m−2 d−1)† 104 (26.1) 23.3 (3.5) 28.2 <0.0001 11.7 <0.0001 CCA (% cover)† 18.1 (7.5) 1.51 (0.8) 21.4 <0.0001 10.1 <0.0001 Non-calcifying algae (% cover) 27.7 (16.0) 57.5 (14.8) 10.9 = 0.0004 5.84 <0.0001 ∗Rank transformation applied to data to meet assumptions of ANOVA. †Square-root transformation applied to data to meet assumptions of ANOVA.

The lower percentage cover by CCA and higher mean percentage cover by non-calcifying algae in the treatment mesocosms compared with controls indicate that CCA may be less competitive for space in a high-pCO2 world, possibly accelerating the shift from dominance by calcifying organisms to fleshy algae observed on many reefs today29. However, the effects of ocean acidification on coverage by fleshy algae will depend on complexities that we did not address in our experiment. Although our study did show an increase in coverage by non-calcifying algae on cylinders in the treatment mesocosms, we did not attempt to

replicate the natural compliment of herbivores found on Hawaiian reef flats, and thus only microherbivores (for example sea hares and amphipods) were in abundance. The variance in percentage cover by non-calcifying algae found on our cylinders was high within treatment (Fig. 2d), indicating that there were undoubtedly factors other than carbonate saturation state and competition with calcifying algae controlling this variable. Further, at the end of our nine-month study, we did not see any patterns in total (entire mesocosm) fleshy algal abundance or biomass related to treatment, whereas we did see the same inhibition of CCA as on

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the cylinders (P.L.J. et al., manuscript in preparation). It will be necessary to investigate the effects of ocean acidification on the ecological process of herbivory and nutrient availability, two factors important in controlling abundance of fleshy algae29, to understand fully the consequences of decreased coverage by CCA for benthic community structure. However, the projected decreased ability of CCA to recruit and claim space in an ecosystem where competition for hard substratum is keen implies that more substrata will be available for colonization by other benthic organisms.

Under all proposed scenarios1, continuous anthropogenic emissions of CO2 to the atmosphere will result in a continuous decline in the pH and calcium carbonate saturation state of ocean waters, with all the ecological implications of such a change in a major Earth-surface-system carbon reservoir. The only way to slow or prevent the continuing acidification of surface ocean waters is to reduce the emissions of CO2 from human activities to the atmosphere; however, because of the slow mixing rate of the oceans, they will continue to be a major sink of anthropogenic CO2 emissions well into the future, and ocean acidification will continue to intensify. Our study demonstrates that changes in benthic community structure on coral reefs may occur owing to the impact of ocean acidification on ecological processes such as recruitment and competition for space. Extrapolation of experiments measuring decreases in calcification rates by various organisms to predict future reef accretion rates may underestimate the impacts of ocean acidification by failing to account for the replacement of calcifying organisms by those that do not produce calcium carbonate. Predicting changes in community structure resulting from ocean acidification and other stressors (for example high-temperature anomalies) will be important in modelling future rates of carbonate production by coral reefs and associated ecosystems.

METHODS

Six 1×1×0.5-m fibreglass mesocosm tanks were continuously supplied with flowing sea water pumped from 2 m depth at the edge of the coral reef at Moku O Loe (Coconut Island), Kaneohe Bay, Hawaii (21.4◦ N, 157.8◦ W), at a rate of eight litres per min per mesocosm (complete turnover rate ≈ 1 h). Three mesocosms were randomly chosen by role of dice to be maintained at an ambient (control, mean midday±s.d. = 400±47µatm pCO2) chemical state, and the remaining three were maintained at a daytime pCO2 level exceeding control conditions by 365µatm on average. The latter level at midday is near that expected by the end of the 21st century following the business-as-usual IS92a CO2 emission scenario assuming equilibrium between the atmosphere and surface sea water (765±39µatm, Fig. 1a). Note that the pCO2 of Kaneohe Bay and many other coral reef environments, on average, is greater than the overlying atmosphere30. Furthermore, on diurnal timescales, the surface seawater pCO2 may fluctuate significantly owing to changes in reef metabolism between day and night23. Carbonate chemistry was altered with hydrochloric acid diluted with tap water to a 10% solution added at 1.3 ml min−1 by a peristaltic pump to the inflow pipes of each treatment mesocosm (control mesocosms received tap water at the same rate). The amount of tap water added to the inflowing water represents a 0.016% addition and was not enough to affect salinity in the mesocosms. Treatments were initiated in the mesocosms on 31 October 2005. Temperature, salinity, dissolved oxygen and pH were measured and water samples were taken in all six mesocosms at least once per week around midday (10 a.m.–2 p.m. HST). Water samples were analysed for dissolved inorganic carbon and total alkalinity following standard procedures (see the Supplementary Information). Diurnal sampling (every 3 h for 24 h) was conducted on several occasions in order to quantify the daily natural variability in the mesocosms (for example Fig. 1e–h). Between 2 February and 24 March 2006, clear acrylic cylinders were added to the mesocosms (three replicates per mesocosm) in order to provide symmetrical substrata that could be removed and examined for encrusting community recruitment and development. The resulting communities were quantified by taking six non-overlapping

still photographs of cylinder surfaces and tabulating the presence/absence of crustose coralline and non-calcifying algae under randomly distributed points on the image using PhotoGrid (C. Bird, University of Hawaii) software (n = 50 points per image).

Received 25 July 2007; accepted 19 November 2007; published 23 December 2007.

References 1. IPCC. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third

Assessment Report of the Intergovernmental Panel on Climate Change (Cambridge Univ. Press, Cambridge, 2001).

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3. Quay, P. Ups and downs of CO2 uptake. Science 298, 2344 (2002). 4. Sabine, C. L. et al. The oceanic sink for anthropogenic CO2. Science 305, 367–371 (2004). 5. Feely, R. A. et al. Impact of anthropogenic CO2 on the CaCO3 system in the oceans. Science 305,

362–366 (2004). 6. Gattuso, J. P., Allemand, D. & Frankignoulle, M. Photosynthesis and calcification at cellular,

organismal and community levels in coral reefs: A review on interactions and control by carbonate chemistry. Am. Zool. 39, 160–183 (1999).

7. Orr, J. C. et al. Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms. Nature 437, 681–686 (2005).

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9. Leclercq, N., Gattuso, J. P. & Jaubert, J. CO2 partial pressure controls the calcification rate of a coral community. Global Change Biol. 6, 329–334 (2000).

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11. Andersson, A. J., Mackenzie, F. T. & Lerman, A. Coastal ocean and carbonate systems in the high CO2 world of the anthropocene. Am. J. Sci. 305, 875–918 (2005).

12. Chave, K. E. Factors influencing the mineralogy of carbonate sediments. Limnol. Oceanogr. 7, 218–223 (1962).

13. Adey, W. H. & Macintyre, I. G. Crustose coralline algae: A re-evaluation in the geological sciences. Geol. Soc. Am. Bull. 84, 883–904 (1973).

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15. Littler, M. M., Littler, D. S., Blair, S. M. & Norris, J. N. Deepest known plant life discovered on an uncharted seamount. Science 227, 57–59 (1985).

16. Adey, W. H. Coral reefs: Algal structured and mediated ecosystems in shallow, turbulent, alkaline waters. J. Phycol. 34, 393–406 (1998).

17. Morse, D. E., Hooker, N., Morse, A. N. C. & Jensen, R. A. Control of larval metamorphosis and recruitment in sympatric agariciid corals. J. Exp. Mar. Biol. Ecol. 116, 193–217 (1988).

18. Heyward, A. J. & Negri, A. P. Natural inducers for coral larval metamorphosis. Coral Reefs 18, 273–279 (1999).

19. Marubini, F., Ferrier-Pages, C. & Cuif, J. P. Suppression of skeletal growth in scleractinian corals by decreasing ambient carbonate-ion concentration: A cross-family comparison. Proc. R. Soc. Lond. B 270, 179–184 (2003).

20. Mackenzie, F. T. & Agegian, C. R. in Origin, Evolution, and Modern Aspects of Biomineralization in Plants and Animals (ed. Crick, R. E.) 11–27 (Plenum, New York, 1989).

21. Gao, K. et al. Calcification in the articulated coralline alga Corallina pilulifera, with special reference to the effect of elevated CO2 concentration. Mar. Biol. 117, 129–132 (1993).

22. Gattuso, J. P., Frankignoulle, M., Bourge, I., Romaine, S. & Buddemeier, R. W. Effect of calcium carbonate saturation of seawater on coral calcification. Global Planet. Change 18, 37–46 (1998).

23. Ohde, S. & Van Woesik, R. Carbon dioxide flux and metabolic processes of a coral reef, Okinawa. Bull. Mar. Sci. 65, 559–576 (1999).

24. Cohen, A. L. & McConnaughey, T. A. in Biomineralization, Reviews in Mineralogy and Geochemistry Vol. 54 (eds Dove, P. M., De Yoreo, J. J. & Weiner, S.) 151–187 (Mineralogical Society of America, 2003).

25. Agegian, C. R. The Biogeochemical Ecology of Porolithon Gardineri (Foslie). Dissertation, Univ. Hawaii (1985).

26. Mackenzie, F. T. et al. Magnesian calcites: Low-temperature occurrence, solubility and solid-solution behavior. Rev. Mineral. Geochem. 11, 97–144 (1983).

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28. Morse, J. W., Andersson, A. J. & Mackenzie, F. T. Initial responses of carbonate-rich shelf sediments to rising atmospheric pCO2 and “ocean acidification”: Role of high Mg-calcites. Geochim. Cosmochem. Acta 70, 5814–5830 (2006).

29. McCook, L. J. Macroalgae nutrients and phase shifts on coral reefs: Scientific issues and management consequences for the Great Barrier Reef. Coral Reefs 18, 357–367 (1999).

30. Fagan, K. E. & Mackenzie, F. T. Air–sea CO2 exchange in a subtropical estuarine-coral reef system, Kaneohe Bay, Oahu, Hawaii. Mar. Chem. 106, 174–191 (2007).

Acknowledgements Support for I.B.K.’s efforts on the project was provided by the USGS Terrestrial, Freshwater and Marine Ecosystems program and the USGS Coastal and Marine Geology Program. A.J.A. and F.T.M. were funded by NSF. The contributions of P.L.J. and K.S.R. were supported by the USGS, EPA Star and the NOAA National Ocean Service. We thank R. Solomon, E. DeCarlo, C. Sabine and R. Feely for permission to include the CRIMP/CO2-NOAA PMEL buoy pCO2 data in Fig. 1. Any use of trade names herein was only for descriptive purposes and does not imply endorsement by the US Government. Correspondence and requests for materials should be addressed to I.B.K. or A.J.A. Supplementary Information accompanies this paper on www.nature.com/naturegeoscience.

Author contributions I.B.K., A.J.A., P.L.J. and F.T.M. contributed equally to the design and I.B.K., A.J.A. and K.S.R. contributed equally to carrying out the experiments. All authors contributed to data synthesis and writing of the manuscript.

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  • Decreased abundance of crustose coralline algae due to ocean acidification
    • Main
    • Methods
    • Acknowledgements
    • References

Vegan Diet

Topic: Veganism, Vegan diet

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PowerPoint Presentation On Pneumococcal Meningitis

Do a topic on Pneumococcal Meningitis, topic should be 15 minute presentation.

Reflect current knowledge of the selected relevant topic.

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